text:
2002, GEOPHYS RES LETT, V29, DOI 10.1029/2002GL015075.
   New M, 2000, J CLIMATE, V13, P2217, DOI 10.1175/1520-0442(2000)013<2217:RTCSTC>2.0.CO;2.
   Nichols EF, 1893, PHYS REV, V1, P1.
   Nicholson SE, 2000, INT J CLIMATOL, V20, P1761, DOI 10.1002/1097-0088(20001130)20:14\<1761::AID-JOC580\>3.0.CO;2-W.
   Nicholson SE, 2000, J CLIMATE, V13, P2628, DOI 10.1175/1520-0442(2000)013<2628:AAORRC>2.0.CO;2.
   NICHOLSON SE, 1993, J CLIMATE, V6, P1463, DOI 10.1175/1520-0442(1993)006<1463:AOOARF>2.0.CO;2.
   Nicholson SE, 2001, INT J CLIMATOL, V21, P1733, DOI 10.1002/joc.648.
   Nicholson SE, 2001, CLIM RES, V17, P123, DOI 10.3354/cr017123.
   Osman YZ, 2002, INT J CLIMATOL, V22, P1861, DOI 10.1002/joc.860.
   Paeth H, 2003, METEOROL Z, V12, P157, DOI 10.1127/0941-2948/2003/0012-0157.
   PAETH H, 2004, IN PRESS MAUSAM.
   PAETH H, 2004, IN PRESS CLIMATIC CH.
   Poccard I, 2000, CLIM DYNAM, V16, P897, DOI 10.1007/s003820000087.
   Rayner N.A., 1996, 74 CRTN.
   Rodriguez-Fonseca B, 2002, GEOPHYS RES LETT, V29, DOI 10.1029/2001GL014421.
   ROECKNER E, 1996, 218 M PLANCK I MET.
   ROWELL DP, 1995, Q J ROY METEOR SOC, V121, P669, DOI 10.1256/smsqj.52310.
   Rowell DP, 2003, J CLIMATE, V16, P849, DOI 10.1175/1520-0442(2003)016\<0849:TIOMSO\>2.0.CO;2.
   Ruiz-Barradas A, 2000, J CLIMATE, V13, P3285, DOI 10.1175/1520-0442(2000)013<3285:SOITDC>2.0.CO;2.
   SAHA K, 2001, MAUSAM, V52, P479.
   Saravanan R, 2000, J CLIMATE, V13, P2177, DOI 10.1175/1520-0442(2000)013<2177:IBTAVA>2.0.CO;2.
   SCHNITZLER KG, 2001, 329 M PLANCK I MET, P13.
   Semazzi FHM, 2001, CLIMATE RES, V17, P169, DOI 10.3354/cr017169.
   Su H, 2001, J GEOPHYS RES-ATMOS, V106, P20025, DOI 10.1029/2000JD000124.
   Sutton RT, 2000, J CLIMATE, V13, P3261, DOI 10.1175/1520-0442(2000)013<3261:TEOCVI>2.0.CO;2.
   Vizy EK, 2001, J CLIMATE, V14, P795, DOI 10.1175/1520-0442(2001)014<0795:MBWGOG>2.0.CO;2.
   von Storch H, 1984, STAT ANAL CLIMATE RE, DOI {[}10.1017/CBO9780511612336, DOI 10.1017/CBO9780511612336].
   Wang GL, 2000, GEOPHYS RES LETT, V27, P795, DOI 10.1029/1999GL011089.
   Zeng N, 1999, SCIENCE, V286, P1537, DOI 10.1126/science.286.5444.1537.}},
Number-of-Cited-References = {{59}},
Times-Cited = {{41}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{14}},
Journal-ISO = {{Clim. Dyn.}},
Doc-Delivery-Number = {{886CS}},
Unique-ID = {{ISI:000226205100010}},
DA = {{2020-08-06}},
}

@article{ ISI:000226382900002,
Author = {Ulanowicz, RE},
Title = {{Quantitative methods for ecological network analysis}},
Journal = {{COMPUTATIONAL BIOLOGY AND CHEMISTRY}},
Year = {{2004}},
Volume = {{28}},
Number = {{5-6}},
Pages = {{321-339}},
Month = {{DEC}},
Abstract = {{The analysis of networks of ecological trophic transfers is a useful
   complement to simulation modeling in the quest for understanding
   whole-ecosystem dynamics. Trophic networks can be studied in
   quantitative and systematic fashion at several levels. Indirect
   relationships between any two individual taxa in an ecosystem, which
   often differ in either nature or magnitude from their direct influences,
   can be assayed using techniques from linear algebra. The same
   mathematics can also be employed to ascertain where along the trophic
   continuum any individual taxon is operating, or to map the web of
   connections into a virtual linear chain that summarizes trophodynamic
   performance by the system. Backtracking algorithms with pruning have
   been written which identify pathways for the recycle of materials and
   energy within the system. The pattern of such cycling often reveals
   modes of control or types of functions exhibited by various groups of
   taxa. The performance of the system as a whole at processing material
   and energy can be quantified using information theory. In particular,
   the complexity of process interactions can be parsed into separate terms
   that distinguish organized, efficient performance from the capacity for
   further development and recovery from disturbance. Finally, the
   sensitivities of the information-theoretic system indices appear to
   identify the dynamical bottlenecks in ecosystem functioning. (C) 2004
   Elsevier Ltd. All fights reserved.}},
Publisher = {{ELSEVIER SCI LTD}},
Address = {{THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND}},
Type = {{Review}},
Language = {{English}},
Affiliation = {{Ulanowicz, RE (Corresponding Author), Univ Maryland, Ctr Environm Sci, Chesapeake Biol Lab, Solomons, MD 20688 USA.
   Univ Maryland, Ctr Environm Sci, Chesapeake Biol Lab, Solomons, MD 20688 USA.}},
DOI = {{10.1016/j.compbiolchem.2004.09.001}},
ISSN = {{1476-9271}},
EISSN = {{1476-928X}},
Keywords = {{ascendency; cycling in ecosystems; ecosystem status; flow networks;
   information theory; input-output analysis; nutrient limitation; trophic
   levels}},
Keywords-Plus = {{ECOSYSTEM FLOW NETWORKS; USER-FRIENDLY TOOL; TROPHIC LEVELS;
   STEADY-STATE; FOOD WEBS; INFORMATION; DYNAMICS; SYSTEMS; ENERGY;
   ORGANIZATION}},
Research-Areas = {{Life Sciences \& Biomedicine - Other Topics; Computer Science}},
Web-of-Science-Categories  = {{Biology; Computer Science, Interdisciplinary Applications}},
Author-Email = {{ulan@cbl.umces.edu}},
ResearcherID-Numbers = {{Ulanowicz, Robert E/G-1021-2013}},
Cited-References = {{ABRAMSON N, 1963, INFORMATION THEORY C.
   Allesina S, 2004, COMPUT BIOL CHEM, V28, P227, DOI 10.1016/j.compbiolchem.2004.04.002.
   Allesina S, 2004, ENVIRON MODELL SOFTW, V19, P337, DOI 10.1016/j.envsoft.2003.10.002.
   Allesina S, 2003, ECOL MODEL, V165, P221, DOI 10.1016/S0304-3800(03)00075-9.
   ALLESINA S, ECOLOGICAL SUBSYSTEM.
   ATLAN H, 1974, J THEOR BIOL, V45, P295, DOI 10.1016/0022-5193(74)90115-5.
   AUGUSTINOVICS M, 1970, CONTRIBUTIONS INPUT, V1, P249.
   Baird D, 2004, ECOL APPL, V14, P805, DOI 10.1890/02-5094.
   BAIRD D, 1989, ECOL MONOGR, V59, P329, DOI 10.2307/1943071.
   BAIRD D, 1991, PHILOS T R SOC B, V333, P15, DOI 10.1098/rstb.1991.0058.
   Bersier LF, 2002, ECOLOGY, V83, P2394, DOI 10.1890/0012-9658(2002)083{[}2394:QDOFWM]2.0.CO;2.
   BLACHMAN NM, 1961, P IRE, V49, P1331.
   Bondavalli C, 1999, ECOSYSTEMS, V2, P49, DOI 10.1007/s100219900057.
   CHRISTENSEN V, 1992, ECOL MODEL, V61, P169, DOI 10.1016/0304-3800(92)90016-8.
   Christian RR, 1999, ECOL MODEL, V117, P99, DOI 10.1016/S0304-3800(99)00022-8.
   CHRISTIAN RR, 2003, 2003343E UNCWRRI E C.
   COHEN JE, 1990, COMMUNITY FOOD WEBS, V20.
   Courant R., 1936, DIFFERENTIAL INTEGRA, V2.
   COUSINS S, 1985, NEW SCI, V107, P50.
   Depew D., 1994, DARWINISM EVOLVING S.
   Fath BD, 2004, ENVIRON MODELL SOFTW, V19, P341, DOI 10.1016/j.envsoft.2003.11.001.
   Fath BD, 1998, ECOL MODEL, V107, P127, DOI 10.1016/S0304-3800(97)00213-5.
   Fath BD, 1999, ECOSYSTEMS, V2, P167, DOI 10.1007/s100219900067.
   FATH BD, MATLAB FUNCTION NETW.
   FINN JT, 1976, J THEOR BIOL, V56, P363, DOI 10.1016/S0022-5193(76)80080-X.
   FISCUS DA, 2002, ESA B, V83, P94.
   Han BP, 1997, ECOL MODEL, V104, P289, DOI 10.1016/S0304-3800(97)00137-3.
   HANNON B, 1973, J THEOR BIOL, V41, P535, DOI 10.1016/0022-5193(73)90060-X.
   HANNON B, 1991, THEOR POPUL BIOL, V40, P78, DOI 10.1016/0040-5809(91)90047-J.
   Heymans J. J., 2003, ECOSYSTEM MODELS NEW, V11, P62.
   Higashi M., 1991, THEORETICAL STUDIES, P117.
   HIGASHI M, 1991, THEORETICAL STUDIES.
   HILLEBRAND H, AQUATIC FOOD WEBS EC, pCH14.
   Holling C. S., 1986, SUSTAINABLE DEV BIOS, P292.
   KARR JR, 1986, ILLINOIS NATURAL HIS, V5.
   KAUFFMAN SA, 1991, SCI AM, V265, P78, DOI 10.1038/scientificamerican0891-78.
   Kavanagh P, 2004, ECOL MODEL, V172, P141, DOI 10.1016/j.ecolmodel.2003.09.004.
   KIKAWADA H, 1998, THESIS U MARYLAND CO.
   Knuth D. E., 1973, FUNDAMENTAL ALGORITH, V1.
   Krivov S, 2003, BIOSYSTEMS, V69, P39, DOI 10.1016/S0303-2647(03)00003-0.
   KULLBACK S, 1959, INFORMATION THEORY S.
   Latham LG, 2002, ECOL MODEL, V154, P25, DOI 10.1016/S0304-3800(02)00032-7.
   LEONTIEF W, 1951, STRUCTURE AM EC.
   LEVINE S, 1980, J THEOR BIOL, V83, P195, DOI 10.1016/0022-5193(80)90288-X.
   LORENZ EN, 1963, J ATMOS SCI, V20, P130, DOI 10.1175/1520-0469(1963)020<0130:DNF>2.0.CO;2.
   MACARTHUR R, 1955, ECOLOGY, V36, P533, DOI 10.2307/1929601.
   Mateti P., 1976, SIAM Journal on Computing, V5, P90, DOI 10.1137/0205007.
   Matis J.H., 1979, COMPARTMENTAL ANAL E, P368.
   MATIS JH, 1981, B INT STAT I, V48, P527.
   MAY RM, 1972, NATURE, V238, P413, DOI 10.1038/238413a0.
   Mueller F., 1998, ECO TARGETS GOAL FUN.
   NAESS A, 1988, ECOLOGIST, V18, P128.
   {*}NSF, 1999, NSF B BALLST VA, V9914.
   ODUM EP, 1969, SCIENCE, V164, P262, DOI 10.1126/science.164.3877.262.
   Odum H.T., 1971, ENV POWER SOC.
   PAHLWOSTL C, 1995, DYNAMIC NATURE ECOSY.
   Pattern B.C., 1976, P457.
   PATTEN BC, 1981, AM NAT, V117, P893, DOI 10.1086/283777.
   PATTEN BC, 1985, ECOL MODEL, V28, P1, DOI 10.1016/0304-3800(85)90013-4.
   PATTEN BC, 1978, OHIO J SCI, V78, P206.
   PATTEN BC, 1982, AM NAT, V119, P179, DOI 10.1086/283903.
   PATTEN BC, 1982, 3 INT C STAT ART EC.
   PIMM SL, 1977, NATURE, V268, P329, DOI 10.1038/268329a0.
   Pimm SL., 1982, FOOD WEBS.
   Platt T., 1981, MATH MODELS BIOL OCE.
   POLIS GA, 1995, FOOD WEBS INTEGRATIO.
   POLOVINA JJ, 1985, FISH B-NOAA, V83, P457.
   RUTLEDGE RW, 1976, J THEOR BIOL, V57, P355, DOI 10.1016/0022-5193(76)90007-2.
   SHEFFER M, 1994, HYDROBIOLOGIA, P275.
   SIMON HA, 1949, ECONOMETRICA, V17, P245.
   SZYRMER J, 1987, ECOL MODEL, V35, P123, DOI 10.1016/0304-3800(87)90094-9.
   Tarjan R., 1972, SIAM Journal on Computing, V1, P146, DOI 10.1137/0201010.
   TILLY LJ, 1968, ECOL MONOGR, V38, P169, DOI 10.2307/1942291.
   TRIBUS M, 1971, SCI AM, V225, P179, DOI 10.1038/scientificamerican0971-179.
   ULANOWICZ R E, 1990, Coenoses, V5, P7.
   Ulanowicz R.E., 1986, GROWTH DEV ECOSYSTEM.
   Ulanowicz R.E., 1984, FLOWS ENERGY MAT MAR, P23.
   Ulanowicz R. E., 1997, ECOLOGY ASCENDANT PE.
   Ulanowicz R. E., 2000, SERIES LANDSCAPE ECO, P113.
   ULANOWICZ RE, 1983, MATH BIOSCI, V65, P219, DOI 10.1016/0025-5564(83)90063-9.
   ULANOWICZ RE, 1979, AM NAT, V114, P871, DOI 10.1086/283534.
   ULANOWICZ RE, 1980, J THEOR BIOL, V85, P223, DOI 10.1016/0022-5193(80)90019-3.
   Ulanowicz RE, 1999, J MARINE SYST, V19, P159, DOI 10.1016/S0924-7963(98)90017-3.
   Ulanowicz RE, 2002, BIOSYSTEMS, V64, P13, DOI 10.1016/S0303-2647(01)00170-8.
   Ulanowicz RE, 1999, BIOSYSTEMS, V50, P127, DOI 10.1016/S0303-2647(98)00097-5.
   ULANOWICZ RE, 1990, INT J SYST SCI, V21, P429, DOI 10.1080/00207729008910372.
   ULANOWICZ RE, 1991, MATH BIOSCI, V103, P45, DOI 10.1016/0025-5564(91)90090-6.
   Ulanowicz RE, 1997, ECOL MODEL, V95, P1, DOI 10.1016/S0304-3800(96)00032-4.
   ULANOWICZ RE, UNPUB LEAST INFERENC.
   ULANOWICZ RE, 1997, UMCESCBL97075 SOL MD.
   ULANOWICZ RE, 1979, THEORETICAL SYSTEMS, P107.
   ULANOWICZ RE, THERMODYNAMICS LIFE, P57.
   Ulanowicz Robert E., 1995, P549.
   Ulanowicz Robert E., 2000, P99.
   VEZINA AF, 1988, MAR ECOL PROG SER, V42, P269, DOI 10.3354/meps042269.
   VONLIEBIG J, 1854, CHEM ITS APPL AGR PH.
   WAGENSBERG J, 1990, B MATH BIOL, V52, P733, DOI 10.1007/BF02460806.
   WHIPPLE SJ, 1993, J THEOR BIOL, V163, P393, DOI 10.1006/jtbi.1993.1127.
   WOODWELL GM, 1969, US BROOKH S BIOL NEW, V22.
   WULFF F, 1989, FLOW ANAL MARINE ECO.
   WULFF F, 1989, FLOW ANAL MARINE ECO, P232.
   YODZIS P, 1989, TRENDS ECOL EVOL, V4, P49, DOI 10.1016/0169-5347(89)90140-7.
   Zorach A. C., 2003, Complexity, V8, P68, DOI 10.1002/cplx.10075.}},
Number-of-Cited-References = {{103}},
Times-Cited = {{263}},
Usage-Count-Last-180-days = {{4}},
Usage-Count-Since-2013 = {{107}},
Journal-ISO = {{Comput. Biol. Chem.}},
Doc-Delivery-Number = {{888OA}},
Unique-ID = {{ISI:000226382900002}},
DA = {{2020-08-06}},
}

@article{ ISI:000226227100007,
Author = {Yi, HS and Hau, JL and Ukidwe, NU and Bakshi, BR},
Title = {{Hierarchical thermodynamic metrics for evaluating the environmental
   sustainability of industrial processes}},
Journal = {{ENVIRONMENTAL PROGRESS}},
Year = {{2004}},
Volume = {{23}},
Number = {{4}},
Pages = {{302-314}},
Month = {{DEC}},
Abstract = {{Industrial progress toward sustainability requires meaningful practical,
   and scientifically sound metrics. Most existing metrics rely on
   information about material and energy inputs and emissions from the main
   process and selected processes in its life cycle. Such metrics often
   result in multiple conflicting variables, making it difficult to use
   them for decision making. Furthermore, sustainability metrics need to be
   scientifically rigorous and capable of evaluating the broader economy
   and ecosystem scale impacts of selected processes and products. This
   paper proposes a framework for evaluating the environmental
   sustainability of industrial processes that satisfies these needs. This
   framework uses energy analysis to combine different types of material
   and energy streams in a thermodynamically sound manner. Energy analysis
   is also combined with end-point life-cycle impact assessment methods for
   evaluating the impact of emissions. This results in metrics for a
   selected system with different levels of aggregation ranging from
   multiple to single dimensions. The challenge of analyzing a process at
   life cycle and coarser spatial scales is met by combining energy
   analysis, life cycle assessment, input-output analysis, and both
   economic and ecological aspects. The result is a doubly nested
   hierarchy, which analyzes processes at multiple spatial scales of
   process, life cycle, economy, and ecosystem. Each scale contains another
   hierarchy based on the degree of aggregation of the metrics. A case
   study of the ammonia process illustrates the characteristics of the
   proposed approach. (C) 2004 American Institute of Chemical Engineers
   Environ Prog.}},
Publisher = {{WILEY}},
Address = {{111 RIVER ST, HOBOKEN, NJ 07030 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Bakshi, BR (Corresponding Author), Ohio State Univ, Dept Chem Engn, Columbus, OH 43210 USA.
   Ohio State Univ, Dept Chem Engn, Columbus, OH 43210 USA.}},
DOI = {{10.1002/ep.10049}},
ISSN = {{0278-4491}},
Keywords-Plus = {{EXERGY; FRAMEWORK}},
Research-Areas = {{Engineering; Environmental Sciences \& Ecology}},
Web-of-Science-Categories  = {{Engineering, Environmental; Engineering, Chemical; Environmental
   Sciences}},
Author-Email = {{bakshi.2@osu.edu}},
ResearcherID-Numbers = {{Bakshi, Bhavik/G-3878-2012
   }},
ORCID-Numbers = {{Bakshi, Bhavik/0000-0002-6604-8408}},
Cited-References = {{{[}Anonymous], 1998, 14041 ISO.
   ARONS JD, 2004, EFFICIENCY SUSTAINAB.
   Ayres RU, 1998, ENERGY, V23, P355, DOI 10.1016/S0360-5442(97)00076-5.
   AYRES RU, 1994, INFORMATION ENTROPY.
   Azapagic A, 2000, PROCESS SAF ENVIRON, V78, P243, DOI 10.1205/095758200530763.
   Bakshi BR, 2003, AICHE J, V49, P1350, DOI 10.1002/aic.690490602.
   Bakshi BR, 2002, COMPUT CHEM ENG, V26, P269, DOI 10.1016/S0098-1354(01)00745-1.
   Bare JC, 2000, INT J LIFE CYCLE ASS, V5, P319, DOI 10.1007/BF02978665.
   Bejan A., 1996, THERMAL DESIGN OPTIM.
   BERTHIAUME R, 2001, EXERGY INT J, V1, P256.
   Dewulf J, 2000, GREEN CHEM, V2, P108, DOI 10.1039/b000015i.
   Dincer I, 2000, ENERG SOURCE, V22, P723, DOI 10.1080/00908310050120272.
   Ekins P, 2003, ECOL ECON, V44, P165, DOI 10.1016/S0921-8009(02)00272-0.
   Fiksel J, 2003, ENVIRON SCI TECHNOL, V37, P5330, DOI 10.1021/es0344819.
   Ford K. W., 1975, EFFICIENT USE ENERGY.
   GRAEDEL TE, 2002, ENV QUALITY MANAGEME, V11, P21.
   Hau J. L., 2002, THESIS OHIO STATE U.
   Hau JL, 2004, ENVIRON SCI TECHNOL, V38, P3768, DOI 10.1021/es034513s.
   Hendrickson C, 1998, ENVIRON SCI TECHNOL, V32, p184A, DOI 10.1021/es983471i.
   Jimenez-Gonzalez C., 2000, INT J LIFE CYCLE ASS, V5, P153, DOI DOI 10.1007/BF02978615.
   KESTIN J, 1980, ENERGY, V5, P679, DOI 10.1016/0360-5442(80)90088-2.
   Lems S, 2002, GREEN CHEM, V4, P308, DOI 10.1039/b203490p.
   MAPLE RE, 2000, PETROLEUM REFINERY P.
   Marteel AE, 2003, ANNU REV ENV RESOUR, V28, P401, DOI 10.1146/annurev.energy.28.011503.163459.
   MUNOZ JR, 2000, J ENERGY RESOURCES T, V121, P268.
   Odum HT, 1996, ENV ACCOUNTING EMERG.
   Pelligrino J. L., 2000, ENERGY ENV PROFILE U.
   Schwarz J, 2002, CHEM ENG PROG, V98, P58.
   SCHWARZ J, 2000, SUSTAINABILITY METRI.
   Seager TP, 2002, J CLEAN PROD, V10, P225, DOI 10.1016/S0959-6526(01)00040-3.
   SEIDER WD, 2004, PROCESS DESIGN PRINC.
   Shreve R. N., 1977, CHEM PROCESS IND.
   Sikdar SK, 2003, AICHE J, V49, P1928, DOI 10.1002/aic.690490802.
   Suh S, 2004, ENVIRON SCI TECHNOL, V38, P657, DOI 10.1021/es0263745.
   SUSSMAN MV, 1980, AVAILABILITY EXERGY.
   Szargut J., 1988, EXERGY ANAL THERMAL.
   THOMAS J, 2004, CLEAR ADVANTAGE BUIL.
   Ukidwe NU, 2004, ENVIRON SCI TECHNOL, V38, P4810, DOI 10.1021/es035367t.
   WIRDAK C, 2003, GEMI SURVEY EHS METR.
   YI HS, 2004, HIERARCHICAL THERMOD.}},
Number-of-Cited-References = {{40}},
Times-Cited = {{28}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{6}},
Journal-ISO = {{Environ. Prog.}},
Doc-Delivery-Number = {{886KV}},
Unique-ID = {{ISI:000226227100007}},
DA = {{2020-08-06}},
}

@article{ ISI:000226084900006,
Author = {Watanabe, M},
Title = {{Asian jet waveguide and a downstream extension of the North Atlantic
   Oscillation}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2004}},
Volume = {{17}},
Number = {{24}},
Pages = {{4674-4691}},
Month = {{DEC}},
Abstract = {{Anomalous atmospheric fields associated with the North Atlantic
   Oscillation (NAO) are analyzed on interannual and intraseasonal time
   scales in order to examine the extent to which the NAO is a regional
   phenomenon.
   Analyses on the interannual time scale reveal that the NAO signal is
   relatively confined to the Euro-Atlantic sector in December while it
   extends toward East Asia and the North Pacific in February. The
   difference is most clearly seen in the meridional wind anomaly, which
   shows a wave train along the Asian jet, collocated with an anomalous
   vorticity source near the jet entrance. Diagnoses using a linear
   barotropic model indicate that this wave train is interpreted as
   quasi-stationary Rossby waves trapped on the Asian jet waveguide, and
   effectively excited by the anomalous upper-level convergence over the
   Mediterranean Sea. It is found that, when the NAO accompanies the
   Mediterranean convergence ( MC) anomaly, most frequently seen in
   February, the NAO indeed has a much wider horizontal structure than the
   classical picture, rather similar to the Arctic Oscillation. In such
   cases interannual variability of the NAO is tied to the East Asian
   climate variability such that the positive NAO tends to bring a surface
   warming over East Asia.
   Similar results are obtained from an analysis of individual NAO events
   based on low-pass-filtered daily fields, which additionally identified
   that the downstream extension occurs at the decay stage of the NAO event
   and the MC anomaly appears to be induced by the Ekman pumping associated
   with the NAO. The signal of the MC anomaly can be detected even at 5
   days before the peak of the NAO, suggesting that the NAO influence to
   East Asia is predictable to some extent; therefore, monitoring the
   developing NAO event is useful to the medium-range weather forecast in
   East Asian countries.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Watanabe, M (Corresponding Author), Hokkaido Univ, Div Ocean \& Atmospher Sci, Nishi 5,Kita 10, Sapporo, Hokkaido 0600810, Japan.
   Hokkaido Univ, Div Ocean \& Atmospher Sci, Sapporo, Hokkaido 0600810, Japan.}},
DOI = {{10.1175/JCLI-3228.1}},
ISSN = {{0894-8755}},
EISSN = {{1520-0442}},
Keywords-Plus = {{ARCTIC OSCILLATION; HEMISPHERE WINTER; GEOGRAPHICAL-DISTRIBUTION;
   ATMOSPHERIC CIRCULATION; TELECONNECTION PATTERNS; GEOPOTENTIAL HEIGHT;
   PART I; TEMPERATURE; VARIABILITY; CLIMATE}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{hiro@ees.hokudai.ac.jp}},
ResearcherID-Numbers = {{Watanabe, Masahiro/G-8228-2017}},
Cited-References = {{Ambaum MHP, 2001, J CLIMATE, V14, P3495, DOI 10.1175/1520-0442(2001)014<3495:AOONAO>2.0.CO;2.
   BARNSTON AG, 1987, MON WEATHER REV, V115, P1083, DOI 10.1175/1520-0493(1987)115<1083:CSAPOL>2.0.CO;2.
   BRANSTATOR G, 1985, J ATMOS SCI, V42, P2225, DOI 10.1175/1520-0469(1985)042<2225:AOGCMS>2.0.CO;2.
   Branstator G, 2002, J CLIMATE, V15, P1893, DOI 10.1175/1520-0442(2002)015<1893:CTTJSW>2.0.CO;2.
   Christiansen B, 2002, GEOPHYS RES LETT, V29, DOI 10.1029/2002GL015208.
   DelSole T, 2001, J ATMOS SCI, V58, P1341, DOI 10.1175/1520-0469(2001)058<1341:OPPITV>2.0.CO;2.
   Deser C, 2000, GEOPHYS RES LETT, V27, P779, DOI 10.1029/1999GL010945.
   DeWeaver E, 2000, J CLIMATE, V13, P3893, DOI 10.1175/1520-0442(2000)013<3893:ZEDOTN>2.0.CO;2.
   DOLE RM, 1983, MON WEATHER REV, V111, P1567, DOI 10.1175/1520-0493(1983)111<1567:PAOTEN>2.0.CO;2.
   Feldstein SB, 2003, Q J ROY METEOR SOC, V129, P901, DOI 10.1256/qj.02.76.
   Feldstein SB, 2002, Q J ROY METEOR SOC, V128, P775, DOI 10.1256/0035900021643683.
   Feldstein SB, 2000, J CLIMATE, V13, P4430, DOI 10.1175/1520-0442(2000)013<4430:TTPSAC>2.0.CO;2.
   Honda M, 2001, J CLIMATE, V14, P1029, DOI 10.1175/1520-0442(2001)014<1029:ISBTAA>2.0.CO;2.
   HOSKINS BJ, 1993, J ATMOS SCI, V50, P1661, DOI 10.1175/1520-0469(1993)050<1661:RWPOAR>2.0.CO;2.
   Hurrell JW, 1996, GEOPHYS RES LETT, V23, P665, DOI 10.1029/96GL00459.
   HURRELL JW, 1995, SCIENCE, V269, P676, DOI 10.1126/science.269.5224.676.
   Hurrell JW, 1997, CLIMATIC CHANGE, V36, P301, DOI 10.1023/A:1005314315270.
   Itoh H, 2002, GEOPHYS RES LETT, V29, DOI 10.1029/2001GL013978.
   Kalnay E, 1996, B AM METEOROL SOC, V77, P437, DOI 10.1175/1520-0477(1996)077<0437:TNYRP>2.0.CO;2.
   KIMOTO M, 1993, J ATMOS SCI, V50, P2625, DOI 10.1175/1520-0469(1993)050<2625:MFRITN>2.0.CO;2.
   Kimoto M, 2001, GEOPHYS RES LETT, V28, P737, DOI 10.1029/2000GL012377.
   Kodera K, 2003, GEOPHYS RES LETT, V30, DOI 10.1029/2003GL017290.
   KUSHNIR Y, 1989, J ATMOS SCI, V46, P3122, DOI 10.1175/1520-0469(1989)046<3122:LFVITN>2.0.CO;2.
   Monahan AH, 2001, GEOPHYS RES LETT, V28, P1019, DOI 10.1029/2000GL012069.
   Peng SL, 2002, GEOPHYS RES LETT, V29, DOI 10.1029/2001GL014043.
   Rodwell MJ, 1999, NATURE, V398, P320, DOI 10.1038/18648.
   SARDESHMUKH PD, 1988, J ATMOS SCI, V45, P1228, DOI 10.1175/1520-0469(1988)045<1228:TGOGRF>2.0.CO;2.
   Thompson DWJ, 2000, J CLIMATE, V13, P1000, DOI 10.1175/1520-0442(2000)013<1000:AMITEC>2.0.CO;2.
   Thompson DWJ, 1998, GEOPHYS RES LETT, V25, P1297, DOI 10.1029/98GL00950.
   Ting MF, 1996, J CLIMATE, V9, P2614, DOI 10.1175/1520-0442(1996)009<2614:NHTPDE>2.0.CO;2.
   VANLOON H, 1978, MON WEATHER REV, V106, P296, DOI 10.1175/1520-0493(1978)106<0296:TSIWTB>2.0.CO;2.
   Walker G.T., 1932, Memoirs of the Royal Meteorological Society, V4, P53.
   Wallace JM, 2000, Q J ROY METEOR SOC, V126, P791, DOI 10.1256/smsqj.56401.
   WALLACE JM, 1981, MON WEATHER REV, V109, P784, DOI 10.1175/1520-0493(1981)109<0784:TITGHF>2.0.CO;2.
   Wallace JM, 2002, J CLIMATE, V15, P1987, DOI 10.1175/1520-0442(2002)015<1987:TPCOAO>2.0.CO;2.
   Watanabe M, 2004, J CLIMATE, V17, P2119, DOI 10.1175/1520-0442(2004)017<2119:DPOTAO>2.0.CO;2.
   Xie SP, 1999, J METEOROL SOC JPN, V77, P573, DOI 10.2151/jmsj1965.77.2\_573.}},
Number-of-Cited-References = {{37}},
Times-Cited = {{171}},
Usage-Count-Last-180-days = {{5}},
Usage-Count-Since-2013 = {{40}},
Journal-ISO = {{J. Clim.}},
Doc-Delivery-Number = {{884KZ}},
Unique-ID = {{ISI:000226084900006}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000226084900018,
Author = {Feng, S and Hu, Q},
Title = {{Variations in the teleconnection of ENSO and summer rainfall in northern
   China: A role of the Indian summer monsoon}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2004}},
Volume = {{17}},
Number = {{24}},
Pages = {{4871-4881}},
Month = {{DEC}},
Abstract = {{Observational studies have created a dilemma on how El Nino-Southern
   Oscillation ( ENSO) may have affected interannual variations of summer
   rainfall in northern China; some suggested a consistent effect while
   others showed a complete lack of effect. This dilemma is resolved in
   this study, which shows that ENSO has affected the summer rainfall in
   northern China and the effect has varied at multidecadal scales. The
   question of how the ENSO teleconnection with northern China rainfall
   variation was established is addressed, and an answer pointing to the
   Indian summer monsoon as a ``facilitator'' connecting ENSO and northern
   China rainfall variation is examined. The Indian monsoon circulation
   interacted with the regional circulations in northern China in some
   epochs and such interaction was interrupted in other epochs. When the
   interaction was active, the Indian monsoon variations originating from
   ENSO, during El Nino or La Nina, was extended to affect the rainfall
   variation in northern China, creating a teleconnection of ENSO with
   northern China rainfall. When the interaction weakened or was inactive,
   the ENSO effect languished. Additional analyses were done to address the
   related question of why the interactions have alternated. The
   alternation was suggested to result from variations of the large-scale
   circulation in the Eurasian continent. The circulation anomalies showed
   lowering ( rising) 500-hPa geopotential height centered at Mongolia and
   western China in some epochs, enhancing cyclonic ( anticyclonic)
   rotation in mid- and low-level winds and creating ( disrupting) a
   moisture convoy from the Indian monsoon region to northern China and
   synergetic convergence/divergence anomalies in the monsoon region and in
   northern China. Results of this study contribute to the understanding of
   interannual and multidecadal variations of the summer rainfall in the
   semiarid region of northern China.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Hu, Q (Corresponding Author), Univ Nebraska, Sch Nat Resource Sci, Climate \& Bioatmospher Sci Grp, 237 LW Chase Hall, Lincoln, NE 68583 USA.
   Univ Nebraska, Sch Nat Resource Sci, Climate \& Bioatmospher Sci Grp, Lincoln, NE 68583 USA.}},
DOI = {{10.1175/JCLI-3245.1}},
ISSN = {{0894-8755}},
EISSN = {{1520-0442}},
Keywords-Plus = {{ASIAN MONSOON; PACIFIC; IMPACT; PRECIPITATION; VARIABILITY; CIRCULATION;
   REANALYSIS}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{qhu2@unl.edu}},
Cited-References = {{CHELLIAH M, 1999, P 24 CLIM DIAGN PRED, P347.
   Dai A, 1997, J CLIMATE, V10, P2943, DOI 10.1175/1520-0442(1997)010<2943:SOGLPV>2.0.CO;2.
   DING Y, 2003, P INT S CLIM CHANG B, P6.
   Ding Y, 1994, MONSOON CHINA.
   Guo Q. -Y., 1988, J TROPICAL METEOROLO, V4, P53.
   Hu Q, 2001, J CLIMATE, V14, P1323, DOI 10.1175/1520-0442(2001)014<1323:ASMOCS>2.0.CO;2.
   Huang G, 2004, ADV ATMOS SCI, V21, P41, DOI 10.1007/BF02915679.
   Huang RH, 2003, ADV ATMOS SCI, V20, P55, DOI 10.1007/BF03342050.
   Kalnay E, 1996, B AM METEOROL SOC, V77, P437, DOI 10.1175/1520-0477(1996)077<0437:TNYRP>2.0.CO;2.
   Kinter JL, 2002, J CLIMATE, V15, P1203, DOI 10.1175/1520-0442(2002)015<1203:RCITCF>2.0.CO;2.
   Kistler R, 2001, B AM METEOROL SOC, V82, P247, DOI 10.1175/1520-0477(2001)082<0247:TNNYRM>2.3.CO;2.
   Krishnamurthy V, 2000, J CLIMATE, V13, P579, DOI 10.1175/1520-0442(2000)013<0579:IMEROI>2.0.CO;2.
   Kumar KK, 1999, SCIENCE, V284, P2156, DOI 10.1126/science.284.5423.2156.
   Lau KM, 2000, J CLIMATE, V13, P2461, DOI 10.1175/1520-0442(2000)013<2461:DABFCO>2.0.CO;2.
   Lau NC, 2003, J CLIMATE, V16, P3, DOI 10.1175/1520-0442(2003)016<0003:AOVITI>2.0.CO;2.
   Lau NC, 2000, J CLIMATE, V13, P4287, DOI 10.1175/1520-0442(2000)013<4287:IOEOTV>2.0.CO;2.
   NITTA T, 1987, J METEOROL SOC JPN, V65, P373, DOI 10.2151/jmsj1965.65.3\_373.
   Parthasarathy B., 1995, RR065 IND I TROP MET.
   Qian WH, 2001, CLIMATIC CHANGE, V50, P419, DOI 10.1023/A:1010673212131.
   Quan XW, 2003, GLOBAL PLANET CHANGE, V37, P171, DOI 10.1016/S0921-8181(02)00200-X.
   Rayner NA, 2003, J GEOPHYS RES-ATMOS, V108, DOI 10.1029/2002JD002670.
   SHUKLA J, 1983, MON WEATHER REV, V111, P1830, DOI 10.1175/1520-0493(1983)111<1830:TSOALR>2.0.CO;2.
   Slingo J., 1999, EL NINO DECADAL VARI, P103.
   Torrence C, 1999, J CLIMATE, V12, P2679, DOI 10.1175/1520-0442(1999)012<2679:ICITEM>2.0.CO;2.
   Wang B, 2002, J CLIMATE, V15, P386, DOI 10.1175/1520-0442(2002)015<0386:RSOTAP>2.0.CO;2.
   Wang B, 2001, J CLIMATE, V14, P4073, DOI 10.1175/1520-0442(2001)014<4073:IVOTAS>2.0.CO;2.
   WANG SW, 1994, INTRO CLIMATE SYSTEM.
   Wilks DS, 1995, STAT METHODS ATMOSPH.
   YATAGAI A, 1995, J METEOROL SOC JPN, V73, P909, DOI 10.2151/jmsj1965.73.5\_909.
   Ye D.-Z., 1996, STUDY REGULARITY FOR.
   ZHANG JJ, 1983, FUNDAMENTALS MEDIUM.
   Zhang RH, 1999, ADV ATMOS SCI, V16, P229, DOI 10.1007/BF02973084.
   黄荣辉, 1989, Advances in Atmospheric Sciences, V6, P21.}},
Number-of-Cited-References = {{33}},
Times-Cited = {{67}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{18}},
Journal-ISO = {{J. Clim.}},
Doc-Delivery-Number = {{884KZ}},
Unique-ID = {{ISI:000226084900018}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000226628500006,
Author = {Wakabayashi, S and Kawamura, R},
Title = {{Extraction of major teleconnection patterns possibly associated with the
   anomalous summer climate in Japan}},
Journal = {{JOURNAL OF THE METEOROLOGICAL SOCIETY OF JAPAN}},
Year = {{2004}},
Volume = {{82}},
Number = {{6}},
Pages = {{1577-1588}},
Month = {{DEC}},
Abstract = {{Four teleconnection patterns that are possibly associated with the
   anomalous summer climate in Japan and the surrounding regions, were
   extracted by applying empirical orthogonal function and regression
   analyses to stream function anomalies. The two teleconnection patterns
   prevailing over northern Eurasia, especially in early summer, called the
   Europe-Japan (EJ) 1 and EJ2, are linked with the variability of the
   Okhotsk high. The third teleconnection pattern, called the West
   Asia-Japan (WJ), is a stationary wave-train pattern along the
   upper-level subtropical jet from West Asia to the central North Pacific,
   which is possibly excited by the anomalous convective heating of the
   Indian summer monsoon. The final teleconnection pattern is identified
   with the Pacific-Japan (PJ), found by Nitta. Teleconnection indices that
   account for the variability of those patterns are also defined on a
   monthly basis. The PJ and WJ patterns, which are more influential
   teleconnection patterns than the others, are closely related to the
   summer temperature anomalies, especially in northern and western Japan,
   respectively. EJ1 and EJ2 were amplified in several extreme summers, and
   they played a vital role in the cool summer of 2003, along with PJ. A
   combination of two or three teleconnection patterns was also responsible
   for the occurrence of the recent extreme summers. Monitoring the major
   teleconnection patterns is very useful for understanding and forecasting
   the anomalous summer climate in East Asia.}},
Publisher = {{METEOROLOGICAL SOC JAPAN}},
Address = {{C/O JAPAN METEOROLOGICAL AGENCY 1-3-4 OTE-MACHI, CHIYODA-KU, TOKYO,
   100-0004, JAPAN}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Kawamura, R (Corresponding Author), Toyama Univ, Dept Earth Sci, Toyama 9308555, Japan.
   Toyama Univ, Dept Earth Sci, Toyama 9308555, Japan.}},
DOI = {{10.2151/jmsj.82.1577}},
ISSN = {{0026-1165}},
EISSN = {{2186-9057}},
Keywords-Plus = {{WESTERN PACIFIC; NORTH PACIFIC; EAST-ASIA; MONSOON; CIRCULATION;
   MECHANISM; EURASIA; IMPACT; AUGUST}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{kawamura@sci.toyama-u.ac.jp}},
ResearcherID-Numbers = {{Kawamura, Ryuichi/Q-6161-2019
   Kawamura, Ryuichi/D-2434-2010
   }},
ORCID-Numbers = {{Kawamura, Ryuichi/0000-0002-6783-1496}},
Cited-References = {{Enomoto T, 2003, Q J ROY METEOR SOC, V129, P157, DOI 10.1256/qj.01.211.
   Fukutomi Y, 2004, J GEOPHYS RES-ATMOS, V109, DOI 10.1029/2003JD003912.
   Guan ZY, 2003, GEOPHYS RES LETT, V30, DOI 10.1029/2002GL016831.
   Huang R.H., 1987, P INT C GEN CIRC E A, P40.
   Kalnay E, 1996, B AM METEOROL SOC, V77, P437, DOI 10.1175/1520-0477(1996)077<0437:TNYRP>2.0.CO;2.
   Kawamura R, 1998, J METEOROL SOC JPN, V76, P1009, DOI 10.2151/jmsj1965.76.6\_1009.
   Kawamura R, 1996, J METEOROL SOC JPN, V74, P867, DOI 10.2151/jmsj1965.74.6\_867.
   Kawamura R, 1998, J METEOROL SOC JPN, V76, P597, DOI 10.2151/jmsj1965.76.4\_597.
   Krishnan R, 2001, J METEOROL SOC JPN, V79, P851, DOI 10.2151/jmsj.79.851.
   KURIHARA K, 1987, J METEOROL SOC JPN, V65, P237, DOI 10.2151/jmsj1965.65.2\_237.
   MURAKAMI T, 1994, J METEOROL SOC JPN, V72, P719, DOI 10.2151/jmsj1965.72.5\_719.
   NAKAMURA H, 2003, IN PRESS Q J ROY MET, V129.
   NITTA T, 1987, J METEOROL SOC JPN, V65, P373, DOI 10.2151/jmsj1965.65.3\_373.
   NORTH GR, 1982, MON WEATHER REV, V110, P699, DOI 10.1175/1520-0493(1982)110<0699:SEITEO>2.0.CO;2.
   Ogi M, 2003, GEOPHYS RES LETT, V30, DOI 10.1029/2003GL017280.
   WANG Y, 1992, J METEOROL SOC JPN, V70, P929, DOI 10.2151/jmsj1965.70.5\_929.
   WANG YF, 1994, J METEOROL SOC JPN, V72, P269, DOI 10.2151/jmsj1965.72.2\_269.
   Wu RG, 2002, J CLIMATE, V15, P3266, DOI 10.1175/1520-0442(2002)015<3266:ACOTEA>2.0.CO;2.}},
Number-of-Cited-References = {{18}},
Times-Cited = {{95}},
Usage-Count-Last-180-days = {{2}},
Usage-Count-Since-2013 = {{18}},
Journal-ISO = {{J. Meteorol. Soc. Jpn.}},
Doc-Delivery-Number = {{892CX}},
Unique-ID = {{ISI:000226628500006}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000227059600023,
Author = {Wang, HT and Xiao, DQ and Zhu, YG and Wu, Q},
Title = {{Introduction of Chinese LCA software - Green star studio}},
Journal = {{RARE METAL MATERIALS AND ENGINEERING}},
Year = {{2004}},
Volume = {{33}},
Number = {{2}},
Pages = {{89-91}},
Month = {{DEC}},
Abstract = {{A Chinese LCA software package, which follows LCA methodology and data
   documentation format defined by ISO14040f, is briefly introduced. This
   program features a typical Windows graphical user interface, with which
   users can construct a flow chart to denote the life cycle of any product
   system. With a flow chart, users can easily turn to the data
   documentation of each process and the result of computation can be shown
   in the flow chart. Thus, the flow chart plays a central role in
   assessment procedures to make them visual and easily understood. using
   three-kinds of graphic elements, i.e. boxes, links and feedback links,
   users can illustrate a product system with internal loops. And matrix
   algorithm is adopted for LCA computation. Hence, this program can
   manipulate the computation of environmental Input/Output Analysis (IOA)
   as well. The localization of data documentation format is also discussed
   in this paper.}},
Publisher = {{NORTHWEST INST NONFERROUS METAL RESEARCH}},
Address = {{C/O RARE METAL MATERIAL ENGINEERING PRESS, PO BOX 51, XIAN, SHAANXI
   710016, PEOPLES R CHINA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Wang, HT (Corresponding Author), Sichuan Univ, Coll Mat Sci, Chengdu 610064, Peoples R China.
   Sichuan Univ, Coll Mat Sci, Chengdu 610064, Peoples R China.}},
ISSN = {{1002-185X}},
Keywords = {{life cycle assessment; program design; ISO14048}},
Research-Areas = {{Materials Science; Metallurgy \& Metallurgical Engineering}},
Web-of-Science-Categories  = {{Materials Science, Multidisciplinary; Metallurgy \& Metallurgical
   Engineering}},
Author-Email = {{Wanght@scu.edu.cn}},
Cited-References = {{CARLSON R, 2001, 14048 ISO TS, P8.
   SUH S, 2003, INT J LCA, V8, P257, DOI DOI 10.1007/BF02978914.
   1998, 14041 ISO.
   2002, 14048 ISO TS.
   2000, 14042 ISO.
   2000, 14043 ISO.
   1997, 14040 ISO.}},
Number-of-Cited-References = {{7}},
Times-Cited = {{0}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{3}},
Journal-ISO = {{Rare Metal Mat. Eng.}},
Doc-Delivery-Number = {{898ES}},
Unique-ID = {{ISI:000227059600023}},
DA = {{2020-08-06}},
}

@article{ ISI:000208299000001,
Author = {Gren, I. -M. and Wulff, F.},
Title = {{Cost-effective nutrient reductions to coupled heterogeneous marine water
   basins: An application to the Baltic Sea}},
Journal = {{REGIONAL ENVIRONMENTAL CHANGE}},
Year = {{2004}},
Volume = {{4}},
Number = {{4}},
Pages = {{159-168}},
Month = {{DEC}},
Abstract = {{In this paper, the role of nutrient transports between marine basins is
   investigated for cost-effective solutions to predetermined marine basin
   targets. The interdependent advective nutrient transports as well as
   retentions among the seven major marine basins of the Baltic Sea are
   described by input-output analysis. This is in contrast to prior
   economic studies of transboundary water pollution that include only
   direct transport between the basins. The analytical results show that
   the difference in impacts between transport specifications depends
   mainly on the `openness' of the basins, that is, their transports with
   other basins. The application on Baltic Sea shows significant
   differences in costs and policy design between the nutrient transport
   specifications. The reason is that the Sea is characterized by long
   water and nutrient residence times, so relatively large part of
   nutrients are transported among basins.}},
Publisher = {{SPRINGER HEIDELBERG}},
Address = {{TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Gren, IM (Corresponding Author), Natl Inst Econ Res, Box 3116, S-10316 Stockholm, Sweden.
   Gren, I. -M., Natl Inst Econ Res, S-10316 Stockholm, Sweden.
   Gren, I. -M., Beijer Int Inst Ecol Econ, S-10405 Stockholm, Sweden.
   Wulff, F., Stockholm Univ, Dept Syst Ecol, S-10691 Stockholm, Sweden.}},
DOI = {{10.1007/s10113-003-0063-6}},
ISSN = {{1436-3798}},
Keywords = {{Minimum costs; Nitrogen; Phosphorous; Marine transports; Baltic Sea}},
Research-Areas = {{Environmental Sciences \& Ecology}},
Web-of-Science-Categories  = {{Environmental Sciences; Environmental Studies}},
Author-Email = {{Ing-marie.Gren@konj.se}},
Cited-References = {{Barrett S., 1990, OXFORD REV ECON POL, V6, P68.
   Baumol W. J., 1988, THEORY ENV POLICY.
   Brooke A., 1998, GAMS USERS GUIDE.
   Conley DJ, 2002, ENVIRON SCI TECHNOL, V36, P5315, DOI 10.1021/es025763w.
   Eckerberg K, 1996, P WORKSH SEPT 27 28.
   Elmgren R, 2001, AMBIO, V30, P222, DOI 10.1639/0044-7447(2001)030{[}0222:UHIOTB]2.0.CO;2.
   Elmgren R, 2001, SCI INTEGRATED COAST, P15.
   ELOFSSON K, 2002, THESIS SWEDISH U AGR.
   Elofsson K., 2000, WORKING PAPER SERIES, V6.
   Folmer H., 2000, PRINCIPLES ENV RESOU.
   Gren I. M., 1997, Environmental and Resource Economics, V10, P341, DOI 10.1023/A:1026497515871.
   Gren I-M, 1995, BEIJER DISCUSSION PA.
   Gren IM, 2001, ENVIRON RESOUR ECON, V20, P41, DOI 10.1023/A:1017512113454.
   {*}HELCOM, 1998, BALT SEA ENV P, V70.
   Hoel M., 1992, ENVIRON RESOUR ECON, V2, P141, DOI DOI 10.1007/BF00338240.
   Johanesson A, 1996, EAERE 7 C LISS JUN.
   KAITALA V, 1995, SCAND J ECON, V97, P325, DOI 10.2307/3440532.
   Maler K-G, 1991, EC POLICY ENV.
   Markowska A, 1996, 7 ANN C LISB PORT.
   Meeuwig JJ, 2000, CAN J FISH AQUAT SCI, V57, P844, DOI 10.1139/cjfas-57-4-844.
   Savchuk O, 2002, APPENDIX 4 MARE SYNT.
   Savchuk OP, 2002, APPENDIX 2 MARE SYNT.
   Sjoberg B, 2002, APPENDIX 9 MARE SYNT.
   WULFF F, 1990, AMBIO, V19, P126.
   Wulff F, 2001, AMBIO, V30, P254, DOI 10.1639/0044-7447(2001)030{[}0254:GAOCEM]2.0.CO;2.
   Wulff F, 1992, AMBIO, V2, P193.
   Zylics T, 2003, ECOLOGICAL IN PRESS.}},
Number-of-Cited-References = {{27}},
Times-Cited = {{12}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{2}},
Journal-ISO = {{Reg. Envir. Chang.}},
Doc-Delivery-Number = {{V22UB}},
Unique-ID = {{ISI:000208299000001}},
DA = {{2020-08-06}},
}

@article{ ISI:000225363300010,
Author = {Ziv, B and Saaroni, H and Alpert, P},
Title = {{The factors governing the summer regime of the eastern Mediterranean}},
Journal = {{INTERNATIONAL JOURNAL OF CLIMATOLOGY}},
Year = {{2004}},
Volume = {{24}},
Number = {{14}},
Pages = {{1859-1871}},
Month = {{NOV 30}},
Note = {{6th Hellenic Conference on Meteorology, Climatology and Atmospheric
   Physics,, Ioannina, GREECE, SEP 25-28, 2002}},
Organization = {{Univ Ioannina, Dept Phys, Lab Meteorol; Hellen Meteorol Soc}},
Abstract = {{The synoptic scale features over the eastern Mediterranean (EM) for
   July-August are examined using National Centers for Environmental
   Prediction-National Center for Atmospheric Research reanalysis data. The
   region is subjected to two primary factors: mid-upper level subsidence
   and lower level cool advection, associated with the Etesian winds.
   The interdiurnal variations of these factors were found to be correlated
   with each other, with a maximum of r = 0.76, found between the 700 hPa
   subsidence and the 925 hPa wind speed. The impact of these factors on
   the temperature regime was examined through their contributions in the
   temperature tendency equation at 32.5 degreesN, 35 degreesE. A
   significant correlation was found between them at the 850 hPa level,
   indicating that they tend to balance each other. This explains the low
   interdiurnal temperature variations there in summer.
   Zonal-vertical and isentropic cross-sections indicate the existence of a
   closed circulation connecting the EM with the Asian monsoon, and a
   meridional-vertical cross-section indicates a signature of the Hadley
   cell across eastern North Africa. Air back-trajectories demonstrate that
   the EM is connected at the lower troposphere with Europe, at the
   midtroposphere with eastern North Africa and at the higher troposphere
   with the Asian monsoon. Significant correlation was found between the
   interdiurnal variations in the upward motion over the Asian monsoon and
   the subsidence over the Levant, with a 1 day lag, implying that the
   Asian monsoon controls the interdiurnal variations over the Levant.
   A detailed analysis shows that the correlation between the two dynamic
   factors governing the EM results from a linkage existing between each
   one of them and the Asian monsoon. An intensification of the Asian
   monsoon enhances both the subsidence over the Levant, via the
   circulation connecting them, and the Etesian winds, due to the enhanced
   pressure gradient between the two regions. Copyright (C) 2004 Royal
   Meteorological Society.}},
Publisher = {{WILEY}},
Address = {{111 RIVER ST, HOBOKEN 07030-5774, NJ USA}},
Type = {{Article; Proceedings Paper}},
Language = {{English}},
Affiliation = {{Ziv, B (Corresponding Author), Open University, Dept Nat Sci, POB 39328, IL-61392 Tel Aviv, Israel.
   Open University, Dept Nat Sci, IL-61392 Tel Aviv, Israel.}},
DOI = {{10.1002/joc.1113}},
ISSN = {{0899-8418}},
EISSN = {{1097-0088}},
Keywords = {{monsoon; Hadley cell; Persian trough; Etesians; Levant; isentropic
   cross-section; subsidence; teleconnection}},
Keywords-Plus = {{ATMOSPHERIC BOUNDARY-LAYER; TEMPORAL BEHAVIOR; ISRAEL; REANALYSIS;
   EXTENSION; CLIMATE; TROUGH}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{baruchz@openu.ac.il}},
Cited-References = {{{*}AIR MIN MET OFF, 1962, WEATH MED, V1.
   ALPERT P, 1990, ISR J EARTH SCI, V39, P93.
   Alpert P, 2004, INT J CLIMATOL, V24, P1001, DOI 10.1002/joc.1036.
   BARRY RG, 1998, AFRICAN MANSOON ATMO.
   BITAN A, 1992, INT J CLIMATOL, V12, P733, DOI 10.1002/joc.3370120706.
   Dayan U, 2002, J APPL METEOROL, V41, P447, DOI 10.1175/1520-0450(2002)041<0447:SASVOT>2.0.CO;2.
   Dayan U, 1999, J APPL METEOROL, V38, P830, DOI 10.1175/1520-0450(1999)038<0830:TTBOTA>2.0.CO;2.
   DAYAN U, 1988, J APPL METEOROL, V27, P1382, DOI 10.1175/1520-0450(1988)027<1382:TSATBO>2.0.CO;2.
   ESHEL G, 2002, ISR J EARTH SCI, V51, P157.
   HOLTON J, 1992, RINTRO DYNAMIC METEO.
   Kalnay E, 1996, B AM METEOROL SOC, V77, P437, DOI 10.1175/1520-0477(1996)077<0437:TNYRP>2.0.CO;2.
   Kistler R, 2001, B AM METEOROL SOC, V82, P247, DOI 10.1175/1520-0477(2001)082<0247:TNNYRM>2.3.CO;2.
   KOCH J, 1992, ATMOS ENVIRON A-GEN, V26, P2537, DOI 10.1016/0960-1686(92)90105-T.
   METAXASDA, 1977, B HELLENIC METEOROLO, V2, P30.
   {*}NOAA, 1997, HYSPLIT4 MODEL.
   PREZERAKOS NG, 1984, ARCH METEOR GEOPHY A, V33, P217, DOI 10.1007/BF02257726.
   Rodwell MJ, 1996, Q J ROY METEOR SOC, V122, P1385, DOI 10.1256/smsqj.53407.
   Saaroni H, 2000, INT J CLIMATOL, V20, P191, DOI 10.1002/(SICI)1097-0088(200002)20:2\<191::AID-JOC464\>3.0.CO;2-E.
   Stephens GL, 1996, J CLIMATE, V9, P305, DOI 10.1175/1520-0442(1996)009<0305:GOOUTW>2.0.CO;2.
   WEBSTER PJ, 1994, REV GEOPHYS, V32, P427, DOI 10.1029/94RG01873.}},
Number-of-Cited-References = {{20}},
Times-Cited = {{167}},
Usage-Count-Last-180-days = {{2}},
Usage-Count-Since-2013 = {{20}},
Journal-ISO = {{Int. J. Climatol.}},
Doc-Delivery-Number = {{874PW}},
Unique-ID = {{ISI:000225363300010}},
DA = {{2020-08-06}},
}

@article{ ISI:000225428600006,
Author = {Hung, CW and Hsu, HH and Lu, MM},
Title = {{Decadal oscillation of spring rain in northern Taiwan}},
Journal = {{GEOPHYSICAL RESEARCH LETTERS}},
Year = {{2004}},
Volume = {{31}},
Number = {{22}},
Month = {{NOV 23}},
Abstract = {{This study found that the spring (February-April) rainfall in northern
   Taiwan has fluctuated concurrently with the Pacific Decadal Oscillation
   (PDO) since the early 20th century. It is proposed that this fluctuation
   in spring rain is induced by the tropical sea surface temperature (SST)
   anomaly embedded in the PDO, which has been known to oscillate in
   opposite phase to the SST in the extra-tropical North Pacific. When the
   PDO index is positive (negative), the SST over the tropical
   Central-Eastern Pacific is warmer (colder) than normal, and a low-level
   anti-cyclonic (cyclonic) anomalous flow is induced over the Philippine
   Sea. This anomalous anti-cyclonic (cyclonic) flow results in
   southwesterly (northeasterly) anomalous winds to the east of Taiwan and
   enhances (reduces) the trough extending southwestward from southern
   Japan to northern Taiwan. As a consequence, more (less) spring rain
   occurs in northern Taiwan during the positive (negative) PDO phases.}},
Publisher = {{AMER GEOPHYSICAL UNION}},
Address = {{2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Hung, CW (Corresponding Author), Natl Taiwan Univ, Dept Atmospher Sci, 1,Sec 4,Roosevelt Rd, Taipei 106, Taiwan.
   Natl Taiwan Univ, Dept Atmospher Sci, Taipei 106, Taiwan.
   Cent Weather Bur, Taipei, Taiwan.}},
DOI = {{10.1029/2004GL021344}},
Article-Number = {{L22206}},
ISSN = {{0094-8276}},
EISSN = {{1944-8007}},
Keywords-Plus = {{EAST ASIAN TELECONNECTION; TROPICAL PACIFIC SSTS; INTERDECADAL
   VARIATIONS; SUMMER MONSOON; PART II; ENSO; VARIABILITY; OCEAN; CLIMATE}},
Research-Areas = {{Geology}},
Web-of-Science-Categories  = {{Geosciences, Multidisciplinary}},
Author-Email = {{cwhung@webmail.as.ntu.edu.tw}},
Cited-References = {{Bond NA, 2003, GEOPHYS RES LETT, V30, DOI 10.1029/2003GL018597.
   Chang CP, 2000, J CLIMATE, V13, P4310, DOI 10.1175/1520-0442(2000)013<4310:IAIVOT>2.0.CO;2.
   Chang CP, 2000, J CLIMATE, V13, P4326, DOI 10.1175/1520-0442(2000)013<4326:IAIVOT>2.0.CO;2.
   Chou C, 2004, J CLIMATE, V17, P2195, DOI 10.1175/1520-0442(2004)017<2195:EOTLWA>2.0.CO;2.
   Deser C, 1996, J CLIMATE, V9, P1840, DOI 10.1175/1520-0442(1996)009<1840:UOTVIT>2.0.CO;2.
   Hsu HH, 2001, CLIM DYNAM, V17, P305, DOI 10.1007/s003820000116.
   Jiang ZH, 2003, MON WEATHER REV, V131, P1769, DOI 10.1175//2561.1.
   LATIF M, 1994, SCIENCE, V266, P634, DOI 10.1126/science.266.5185.634.
   Lau NC, 2003, J CLIMATE, V16, P3, DOI 10.1175/1520-0442(2003)016<0003:AOVITI>2.0.CO;2.
   Lau NC, 2000, J CLIMATE, V13, P4287, DOI 10.1175/1520-0442(2000)013<4287:IOEOTV>2.0.CO;2.
   Mantua NJ, 1997, B AM METEOROL SOC, V78, P1069, DOI 10.1175/1520-0477(1997)078<1069:APICOW>2.0.CO;2.
   May R. J., 2003, ATMOS SCI, V31, P199.
   MILLER AJ, 1994, OCEANOGRAPHY, V7, P21, DOI DOI 10.5670/OCEANOG.1994.11.
   Qiu B, 2003, J PHYS OCEANOGR, V33, P2465, DOI 10.1175/2459.1.
   RAYNER NA, 1996, 74 MET OFF CLIM RES.
   Wang B, 2000, J CLIMATE, V13, P1517, DOI 10.1175/1520-0442(2000)013<1517:PEATHD>2.0.CO;2.
   Wang B, 2002, J CLIMATE, V15, P3252, DOI 10.1175/1520-0442(2002)015<3252:PEATPI>2.0.CO;2.
   Zhang RH, 1998, NATURE, V391, P879, DOI 10.1038/36081.
   Zhang Y, 1997, J CLIMATE, V10, P1004, DOI 10.1175/1520-0442(1997)010<1004:ELIV>2.0.CO;2.}},
Number-of-Cited-References = {{19}},
Times-Cited = {{31}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{5}},
Journal-ISO = {{Geophys. Res. Lett.}},
Doc-Delivery-Number = {{875NY}},
Unique-ID = {{ISI:000225428600006}},
OA = {{Green Published}},
DA = {{2020-08-06}},
}

@article{ ISI:000225123100020,
Author = {Lee, SY and Huh, CA and Su, CC and You, CF},
Title = {{Sedimentation in the Southern Okinawa Trough: enhanced particle
   scavenging and teleconnection between the Equatorial Pacific and western
   Pacific margins}},
Journal = {{DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS}},
Year = {{2004}},
Volume = {{51}},
Number = {{11}},
Pages = {{1769-1780}},
Month = {{NOV}},
Abstract = {{Owing to its location, geomorphology and hydrodynamic conditions, the
   southernmost part of the Southern Okinawa Trough (SOT) acts like an
   efficient receptacle for sediments from Taiwan and the East China Sea
   shelf. The high sediment flux coupled with the passage, bifurcation,
   upwelling, swirling and detour of Kuroshio in the SOT area result in
   intense particle scavenging, with sedimentary inventories of Pb-210 and
   (239,240)pU far greater than expected from local atmospheric input and
   in situ water column production. The unusually high inventories, as well
   as the deposition history of Pu isotopes must be explained by advective
   transport of Pu westward from the Marshall Islands, the largest source
   of Pu in the Pacific, by the North Equatorial Current (NEC) followed by
   northward transport of Kuroshio to the SOT area. The high sedimentation
   rate in the SOT area enabled us to differentiate the subsurface peak of
   Pu-239,Pu- 240 resulting from the global fallout maximum in AD 1963 and
   the subsurface maximum of Pu-240/Pu-239 caused by close-in fallout from
   neutron-rich thermonuclear tests conducted by the US during AD 1952-1954
   at the Enewetak and Bikini Atolls. The vertical offset between the
   subsurface peaks of Pu-239,Pu- 240 and Pu-240/Pu-239 in sediments
   suggests that deposition of the Pu-240/Pu-239 maximum preceded that of
   the Pu-239,Pu- 240 maximum by 3-5 yr and that the transit time of the
   Pu-240-enriched Pu from its source (at similar to12degreesN,
   162degreesE) to the SOT area is similar to6yr. The mean velocity of NEC
   thus calculated is similar to0.022 ms(-1). The present is the key to the
   past. This study reveals teleconnection between the Equatorial Pacific
   and the western Pacific margins and suggests that ODP and IMAGES cores
   recently collected from the SOT area holds great promise for the
   reconstruction of high-resolution paleoceanographic records along the
   trajectories of NEC and Kuroshio. (C) 2004 Elsevier Ltd. All rights
   reserved.}},
Publisher = {{PERGAMON-ELSEVIER SCIENCE LTD}},
Address = {{THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Huh, CA (Corresponding Author), Acad Sinica, Inst Earth Sci, POB 1-55,Nankang, Taipei 115, Taiwan.
   Acad Sinica, Inst Earth Sci, Taipei 115, Taiwan.
   Natl Cheng Kung Univ, Dept Earth Sci, Tainan, Taiwan.}},
DOI = {{10.1016/j.dsr.2004.07.008}},
ISSN = {{0967-0637}},
EISSN = {{1879-0119}},
Keywords = {{Cs-137; Pb-210; plutonium isotopes; Okinawa Trough; Kuroshio; North
   Equatorial Current}},
Keywords-Plus = {{EAST CHINA SEA; KUROSHIO; TAIWAN; PB-210; OCEAN; TRANSPORT; ISOTOPES;
   DYNAMICS; CURRENTS; FALLOUT}},
Research-Areas = {{Oceanography}},
Web-of-Science-Categories  = {{Oceanography}},
Author-Email = {{huh@earth.sinica.edu.tw}},
ResearcherID-Numbers = {{Huh, Chih-An/N-4610-2013
   }},
ORCID-Numbers = {{Su, Chih-Chieh/0000-0002-7624-1607}},
Cited-References = {{BERTINE KK, 1986, J ENVIRON RADIOACTIV, V3, P189, DOI 10.1016/0265-931X(86)90025-1.
   BOWEN VT, 1980, EARTH PLANET SC LETT, V49, P411, DOI 10.1016/0012-821X(80)90083-7.
   CARTER MW, 1977, HEALTH PHYS, V33, P55, DOI 10.1097/00004032-197707000-00006.
   Chen CTA, 1998, OCEANOL ACTA, V21, P713, DOI 10.1016/S0399-1784(99)80027-9.
   Chung YC, 2000, CONT SHELF RES, V20, P571, DOI 10.1016/S0278-4343(99)00086-2.
   DIAMOND H, 1960, PHYS REV, V119, P2000, DOI 10.1103/PhysRev.119.2000.
   Donguy JR, 1996, DEEP-SEA RES PT I, V43, P1105, DOI 10.1016/0967-0637(96)00047-7.
   HUH CA, 1990, CONT SHELF RES, V10, P137, DOI 10.1016/0278-4343(90)90027-J.
   Huh CA, 2004, GEOPHYS RES LETT, V31, DOI 10.1029/2004GL019731.
   Huh CA, 1996, J SOUTHE ASIAN EARTH, V14, P373, DOI 10.1016/S0743-9547(96)00072-4.
   Huh CA, 1999, MAR GEOL, V160, P183, DOI 10.1016/S0025-3227(99)00020-1.
   HUH CA, 1987, GEOCHIM COSMOCHIM AC, V51, P1743, DOI 10.1016/0016-7037(87)90352-8.
   Jian ZM, 2000, EARTH PLANET SC LETT, V184, P305, DOI 10.1016/S0012-821X(00)00321-6.
   KREY PW, 1976, P S TRANS NUCL ENV, V39, P671.
   Lallemand SE, 1997, TECTONOPHYSICS, V274, P171, DOI 10.1016/S0040-1951(96)00303-4.
   LEE SY, 2001, THESIS NATL TAIWAN U, P63.
   Liang WD, 2003, DEEP-SEA RES PT II, V50, P1085, DOI 10.1016/S0967-0645(03)00011-0.
   LIN YN, 1991, TERR ATMOS OCIAN SCI, V2, P243.
   Livingston HD, 2001, RADIOACTIV ENVIRONM, V1, P267.
   NAGAYA Y, 1992, J OCEANOGR, V48, P23, DOI DOI 10.1007/BF02234030.
   Nitani H, 1972, KUROSHIO ITS PHYS AS, P129, DOI DOI 10.1016/S0079-6611(99)00004-X.BG-12-781-2015.
   Oguri K, 2000, GEOPHYS RES LETT, V27, P3893, DOI 10.1029/2000GL011690.
   Robison WL, 1999, SCI TOTAL ENVIRON, V238, P311, DOI 10.1016/S0048-9697(99)00145-X.
   Sawada K, 1998, NATURE, V392, P592, DOI 10.1038/33391.
   SENO T, 1993, J GEOPHYS RES-SOL EA, V98, P17941, DOI 10.1029/93JB00782.
   Su CC, 2003, GEOPHYS RES LETT, V30, DOI 10.1029/2003GL018221.
   Su CC, 2002, MAR GEOL, V183, P163, DOI 10.1016/S0025-3227(02)00165-2.
   Tang TY, 1999, J PHYS OCEANOGR, V29, P1353, DOI 10.1175/1520-0485(1999)029<1353:CSFNOT>2.0.CO;2.
   Tang TY, 2000, CONT SHELF RES, V20, P349, DOI 10.1016/S0278-4343(99)00076-X.
   TANG TY, 1993, J OCEANOGR, V49, P193, DOI DOI 10.1007/BF02237288.
   Ujiie H, 1999, MAR MICROPALEONTOL, V37, P23, DOI 10.1016/S0377-8398(99)00010-9.
   {*}WAT RES BUR, 1999, HYGR YB TAIW WAT RES.
   Wong GTF, 2000, CONT SHELF RES, V20, P331.
   Yeh J-C, 1997, TERR ATMOS OCIAN SCI, V8, P141.}},
Number-of-Cited-References = {{34}},
Times-Cited = {{62}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{16}},
Journal-ISO = {{Deep-Sea Res. Part I-Oceanogr. Res. Pap.}},
Doc-Delivery-Number = {{871ID}},
Unique-ID = {{ISI:000225123100020}},
DA = {{2020-08-06}},
}

@article{ ISI:000225006800008,
Author = {Lachniet, MS and Asmerom, Y and Burns, SJ and Patterson, WP and Polyak,
   VJ and Seltzer, GO},
Title = {{Tropical response to the 8200 yr BP cold event? Speleothem isotopes
   indicate a weakened early Holocene monsoon in Costa Rica}},
Journal = {{GEOLOGY}},
Year = {{2004}},
Volume = {{32}},
Number = {{11}},
Pages = {{957-960}},
Month = {{NOV}},
Abstract = {{A delta(18)O monsoon rainfall proxy record from a U-Th-dated Costa Rican
   stalagmite (8840-4920 yr B.P.) documents an early Holocene dry period
   correlative with the high-latitude 8200 yr B.P. cold event. High
   delta(18)O values between ca. 8300 and 8000 yr B.P. demonstrate reduced
   rainfall and a weaker monsoon in Central America. A relatively wetter
   and more stable monsoon was established ca. 7600 yr B.P. The early
   Holocene dry event suggests a tropical-extratropical teleconnection to
   the 8200 yr B.P. cold event and a possible association of isthmian
   rainfall anomalies with high-latitude climate changes. The likely source
   of such a tropical anomaly is a decrease in Atlantic thermohaline
   circulation and atmospheric perturbations associated with drainage of
   proglacial lakes and freshwater discharge into the North Atlantic. A
   weaker monsoon at 8200 yr B.P. may be linked to wetland contraction and
   a decrease in methane observed in Greenland ice cores.}},
Publisher = {{GEOLOGICAL SOC AMER, INC}},
Address = {{PO BOX 9140, BOULDER, CO 80301-9140 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Lachniet, MS (Corresponding Author), Univ Nevada, Dept Geosci, MS-4010, Las Vegas, NV 89154 USA.
   Univ Nevada, Dept Geosci, Las Vegas, NV 89154 USA.
   Univ New Mexico, Dept Earth \& Planetary Sci, Albuquerque, NM 87131 USA.
   Univ Massachusetts, Dept Geosci, Amherst, MA 01003 USA.
   Univ Saskatchewan, Dept Geol Sci, Saskatoon, SK S7N 5E2, Canada.
   Syracuse Univ, Dept Earth Sci, Syracuse, NY 13244 USA.}},
DOI = {{10.1130/G20797.1}},
ISSN = {{0091-7613}},
EISSN = {{1943-2682}},
Keywords = {{Costa Rica; tropics; paleoclimate; 8200 yr BP event; stalagmite; delta
   O-18; Holocene; Central American monsoon; Intertropical Convergence
   Zone; U-Th dating}},
Keywords-Plus = {{FRESH-WATER OUTBURSTS; ABRUPT CLIMATE-CHANGE; THERMOHALINE CIRCULATION;
   INTERANNUAL VARIABILITY; LAST DEGLACIATION; ATLANTIC-OCEAN; HYDROLOGICAL
   CHANGES; CARIBBEAN RAINFALL; LAKE AGASSIZ; RECORD}},
Research-Areas = {{Geology}},
Web-of-Science-Categories  = {{Geology}},
Author-Email = {{matthew.lachniet@ccmail.nevada.edu}},
ResearcherID-Numbers = {{Patterson, William P/J-6473-2012
   Burns, Stephen/H-9419-2013
   }},
ORCID-Numbers = {{Lachniet, Matthew/0000-0001-5250-0144
   Polyak, Victor/0000-0002-2010-1066
   Patterson, William/0000-0003-3387-708X}},
Cited-References = {{Alley RB, 1997, GEOLOGY, V25, P483, DOI 10.1130/0091-7613(1997)025<0483:HCIAPW>2.3.CO;2.
   ASMEROM Y, 1997, 7 ANN VM GOLDSCHM C.
   Baldini JUL, 2002, SCIENCE, V296, P2203, DOI 10.1126/science.1071776.
   Barber DC, 1999, NATURE, V400, P344, DOI 10.1038/22504.
   BARD E, 1990, NATURE, V345, P405, DOI 10.1038/345405a0.
   Burns SJ, 2001, GEOLOGY, V29, P623, DOI 10.1130/0091-7613(2001)029<0623:SEFOFC>2.0.CO;2.
   CHEN JH, 1986, EARTH PLANET SC LETT, V80, P241, DOI 10.1016/0012-821X(86)90108-1.
   Clark PU, 2002, NATURE, V415, P863, DOI 10.1038/415863a.
   Dean WE, 2002, QUATERNARY SCI REV, V21, P1763, DOI 10.1016/S0277-3791(02)00002-1.
   deMenocal P, 2000, SCIENCE, V288, P2198, DOI 10.1126/science.288.5474.2198.
   Enfield DB, 1999, J CLIMATE, V12, P2093, DOI 10.1175/1520-0442(1999)012<2093:TDOCRO>2.0.CO;2.
   {*}FOOD AGR ORG UN, 1985, ROME FOOD AGR ORG UN, V24.
   Gasse F, 2000, QUATERNARY SCI REV, V19, P189, DOI 10.1016/S0277-3791(99)00061-X.
   Giannini A, 2000, J CLIMATE, V13, P297, DOI 10.1175/1520-0442(2000)013<0297:IVOCRE>2.0.CO;2.
   HASTENRATH S, 1984, MON WEATHER REV, V112, P1097, DOI 10.1175/1520-0493(1984)112<1097:IVAACM>2.0.CO;2.
   HODELL DA, 1995, NATURE, V375, P391, DOI 10.1038/375391a0.
   Hughen KA, 1996, NATURE, V380, P51, DOI 10.1038/380051a0.
   {*}INT ATOM EN AG WO, 1999, GLOB NETW IS PRE GNI.
   Kim ST, 1997, GEOCHIM COSMOCHIM AC, V61, P3461, DOI 10.1016/S0016-7037(97)00169-5.
   Lachniet MS, 2002, J HYDROL, V260, P135, DOI 10.1016/S0022-1694(01)00603-5.
   Ludwig KR, 2003, REV MINERAL GEOCHEM, V52, P631, DOI 10.2113/0520631.
   Magny M, 2004, QUATERNARY RES, V61, P181, DOI 10.1016/j.yqres.2003.12.003.
   MANABE S, 1995, NATURE, V378, P165, DOI 10.1038/378165a0.
   Polyak VJ, 2001, SCIENCE, V294, P148, DOI 10.1126/science.1062771.
   POULSON TL, 1969, SCIENCE, V165, P971.
   RAHMSTORF S, 1995, NATURE, V378, P145, DOI 10.1038/378145a0.
   Renssen H, 2001, GEOPHYS RES LETT, V28, P1567, DOI 10.1029/2000GL012602.
   Richards DA, 2003, REV MINERAL GEOCHEM, V52, P407, DOI 10.2113/0520407.
   Rodbell DT, 1999, SCIENCE, V283, P516, DOI 10.1126/science.283.5401.516.
   ROZANSKI K, 1993, CLIMATE CHANGE CONTI.
   Ruhlemann C, 1999, NATURE, V402, P511, DOI 10.1038/990069.
   Stuiver M, 1995, QUATERNARY RES, V44, P341, DOI 10.1006/qres.1995.1079.
   Teller JT, 2002, QUATERNARY SCI REV, V21, P879, DOI 10.1016/S0277-3791(01)00145-7.
   von Grafenstein U, 1998, CLIM DYNAM, V14, P73, DOI 10.1007/s003820050210.
   Waylen PR, 1996, J CLIMATE, V9, P2606, DOI 10.1175/1520-0442(1996)009<2606:IVOMPI>2.0.CO;2.}},
Number-of-Cited-References = {{35}},
Times-Cited = {{65}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{25}},
Journal-ISO = {{Geology}},
Doc-Delivery-Number = {{869TI}},
Unique-ID = {{ISI:000225006800008}},
DA = {{2020-08-06}},
}

@article{ ISI:000225099000008,
Author = {Yang, S and Lau, KM and Yoo, SH and Kinter, JL and Miyakoda, K and Ho,
   CH},
Title = {{Upstream subtropical signals preceding the Asian summer monsoon
   circulation}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2004}},
Volume = {{17}},
Number = {{21}},
Pages = {{4213-4229}},
Month = {{NOV}},
Abstract = {{In this study, the authors address several issues with respect to the
   antecedent signals of the large-scale Asian summer monsoon that were
   earlier identified by Webster and Yang. In particular, they revisit the
   changes in the subtropical upper-tropospheric westerlies preceding the
   monsoon, depict the detailed structure of the monsoon's antecedent
   signals, and investigate the physical processes from the signals to the
   monsoon. They also explore the teleconnection of these signals to
   various large-scale climate phenomena and emphasize the importance of
   the upstream location of the signals relative to the Tibetan Plateau and
   the monsoon.
   Before a strong (weak) Asian summer monsoon, the 200-mb westerlies over
   subtropical Asia are weak (strong) during the previous winter and
   spring. A significant feature of these signals is represented by the
   variability of the Middle East jet stream whose changes are linked to
   the Arctic Oscillation, North Atlantic Oscillation, El Nino-Southern
   Oscillation, and other climate phenomena. When this jet stream
   intensifies and shifts southeastward, cold air intrudes frequently from
   eastern Europe into the Middle East and southwestern Asia. As a result,
   in subtropical Asia, snow and precipitation increase, the ground wetness
   increases, and surface temperature decreases. A strengthening Middle
   East jet stream is also accompanied by increases in both stationary wave
   activity flux and higher-frequency eddy activities. The Tibetan Plateau
   acts to block these westerly activities propagating eastward and
   increase the persistence of the low-temperature anomalies, which in turn
   prolongs the atmospheric signals from winter to spring.
   A strong link is found between the persistent low-temperature anomalies
   and the decrease in geopotential height over southern Asia, including
   the Tibetan Plateau, in spring. The latter indicates a late
   establishment of the South Asian high, and implies a delay in the
   atmospheric transition from winter to summer conditions and in the
   development of the summer monsoon. The preceding scenario for a strong
   Middle East jet stream and a weaker Asian monsoon can be applied
   accordingly for the discussion of the physical processes from a weak jet
   stream to a strong monsoon.
   The current results of the relationship between the extratropical
   process and Asian monsoon resemble several features of the
   tropical-extratropical interaction mechanism for the tropospheric
   biennial oscillation (TBO). While the role of tropical heating is
   emphasized in the TBO mechanism, compared to the variability of the sea
   surface temperature related to El Nino-Southern Oscillation, the
   extratropical process examined in this study is more strongly linked to
   the Asian summer monsoon.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Yang, S (Corresponding Author), NCEP NWS NOAA, Climate Predict Ctr, 5200 Auth Rd,Rm 605, Camp Springs, MD 20746 USA.
   NCEP NWS NOAA, Climate Predict Ctr, Camp Springs, MD 20746 USA.
   NASA, Goddard Space Flight Ctr, Atmospheres Lab, Greenbelt, MD 20771 USA.
   Seoul Natl Univ, Sch Earth \& Environm Sci, Seoul, South Korea.
   Ctr Ocean Land Atmosphere Studies, Calverton, MD USA.}},
DOI = {{10.1175/JCLI3192.1}},
ISSN = {{0894-8755}},
EISSN = {{1520-0442}},
Keywords-Plus = {{TROPOSPHERIC BIENNIAL OSCILLATION; SEA-SURFACE-TEMPERATURE; EURASIAN
   SNOW COVER; TROPICAL-WIDE TELECONNECTION; SPACE-TIME CLIMATE;
   INTERANNUAL VARIABILITY; SOUTHERN-OSCILLATION; TIBETAN PLATEAU; EL-NINO;
   3-DIMENSIONAL PROPAGATION}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{song.yang@noaa.gov}},
ResearcherID-Numbers = {{Yang, Song/B-4952-2009
   Lau, William K/E-1510-2012
   Ho, Chang-Hoi/H-8354-2015}},
ORCID-Numbers = {{Lau, William K/0000-0002-3587-3691
   }},
Cited-References = {{Annamalai H, 1999, MON WEATHER REV, V127, P1157, DOI 10.1175/1520-0493(1999)127<1157:TMEAVO>2.0.CO;2.
   Bamzai AS, 1999, J CLIMATE, V12, P3117, DOI 10.1175/1520-0442(1999)012<3117:RBESCS>2.0.CO;2.
   Banerjee A., 1978, INDIAN J MET HYDROL, V29, P425.
   BARNETT TP, 1989, J ATMOS SCI, V46, P661, DOI 10.1175/1520-0469(1989)046<0661:TEOESC>2.0.CO;2.
   Blandford HF, 1884, P ROY SOC LONDON, V37, P3, DOI {[}10.1098/rspl.1884.0003, DOI 10.1098/RSPL.1884.0003].
   Bolin B., 1950, TELLUS, V2, P184, DOI DOI 10.1111/J.2153-3490.1950.TB00330.X.
   Chang CP, 2000, J ATMOS SCI, V57, P2209, DOI 10.1175/1520-0469(2000)057<2209:ATFTTT>2.0.CO;2.
   Chang CP, 2001, J CLIMATE, V14, P2376, DOI 10.1175/1520-0442(2001)014<2376:PROACO>2.0.CO;2.
   Dugam SS, 1997, THEOR APPL CLIMATOL, V58, P21, DOI 10.1007/BF00867429.
   GADGIL S, 1977, PURE APPL GEOPHYS, V115, P1413, DOI 10.1007/BF00874416.
   Gong DY, 2003, J GEOPHYS RES-ATMOS, V108, DOI 10.1029/2002JD002193.
   Goswami BN, 1999, Q J ROY METEOR SOC, V125, P611, DOI 10.1002/qj.49712555412.
   HAHN DG, 1976, J ATMOS SCI, V33, P2461, DOI 10.1175/1520-0469(1976)033<2461:AARBES>2.0.CO;2.
   Hansen J, 1999, J GEOPHYS RES-ATMOS, V104, P30997, DOI 10.1029/1999JD900835.
   HE HY, 1987, MON WEATHER REV, V115, P1966, DOI 10.1175/1520-0493(1987)115<1966:OOTASM>2.0.CO;2.
   JU JH, 1995, Q J ROY METEOR SOC, V121, P1133, DOI 10.1002/qj.49712152509.
   Kalnay E, 1996, B AM METEOROL SOC, V77, P437, DOI 10.1175/1520-0477(1996)077<0437:TNYRP>2.0.CO;2.
   Kawamura R, 1998, J METEOROL SOC JPN, V76, P1009, DOI 10.2151/jmsj1965.76.6\_1009.
   Lau KM, 1998, CLIM DYNAM, V14, P759, DOI 10.1007/s003820050253.
   Lau KM, 2000, J CLIMATE, V13, P2461, DOI 10.1175/1520-0442(2000)013<2461:DABFCO>2.0.CO;2.
   Lau NC, 2000, J CLIMATE, V13, P4287, DOI 10.1175/1520-0442(2000)013<4287:IOEOTV>2.0.CO;2.
   Li CF, 1996, J CLIMATE, V9, P358, DOI 10.1175/1520-0442(1996)009<0358:TOAIVO>2.0.CO;2.
   LinHo, 2002, J CLIMATE, V15, P2001, DOI 10.1175/1520-0442(2002)015.
   LUO H, 1984, MON WEATHER REV, V112, P966, DOI 10.1175/1520-0493(1984)112<0966:TLSCAH>2.0.CO;2.
   MEEHL GA, 1994, J CLIMATE, V7, P1033, DOI 10.1175/1520-0442(1994)007<1033:IOTLSI>2.0.CO;2.
   Meehl GA, 2002, J CLIMATE, V15, P722, DOI 10.1175/1520-0442(2002)015<0722:TTBOAA>2.0.CO;2.
   MEEHL GA, 1987, MON WEATHER REV, V115, P27, DOI 10.1175/1520-0493(1987)115<0027:TACAIV>2.0.CO;2.
   Meehl GA, 1997, J CLIMATE, V10, P1921, DOI 10.1175/1520-0442(1997)010<1921:TSAMAT>2.0.CO;2.
   Meehl GA, 2002, J CLIMATE, V15, P923, DOI 10.1175/1520-0442(2002)015<0923:IMGSET>2.0.CO;2.
   Miyakoda K, 1999, Q J ROY METEOR SOC, V125, P2937, DOI 10.1256/smsqj.56007.
   Miyakoda K, 2003, J METEOROL SOC JPN, V81, P1015, DOI 10.2151/jmsj.81.1015.
   MOOLEY DA, 1986, J CLIM APPL METEOROL, V25, P633, DOI 10.1175/1520-0450(1986)025<0633:RBISMR>2.0.CO;2.
   MURAKAMI T, 1986, MON WEATHER REV, V114, P1456, DOI 10.1175/1520-0493(1986)114<1456:RASCLF>2.0.CO;2.
   MURAKAMI T, 1982, J METEOROL SOC JPN, V60, P183, DOI 10.2151/jmsj1965.60.1\_183.
   MURAKAMI T, 1987, MONSOON METEOROLOGY.
   Navarra A, 1999, Q J ROY METEOR SOC, V125, P2909, DOI 10.1256/smsqj.56006.
   New M, 1999, J CLIMATE, V12, P829, DOI 10.1175/1520-0442(1999)012<0829:RTCSTC>2.0.CO;2.
   New M, 2000, J CLIMATE, V13, P2217, DOI 10.1175/1520-0442(2000)013<2217:RTCSTC>2.0.CO;2.
   NORMAND C, 1953, Q J ROY METEOR SOC, V79, P463, DOI 10.1002/qj.49707934202.
   Ogasawara N, 1999, J METEOROL SOC JPN, V77, P1247, DOI 10.2151/jmsj1965.77.6\_1247.
   PARTHASARATHY B, 1991, J CLIMATE, V4, P927, DOI 10.1175/1520-0442(1991)004<0927:EOSVII>2.0.CO;2.
   Peterson TC, 1997, B AM METEOROL SOC, V78, P2837, DOI 10.1175/1520-0477(1997)078<2837:AOOTGH>2.0.CO;2.
   PLUMB RA, 1985, J ATMOS SCI, V42, P217, DOI 10.1175/1520-0469(1985)042<0217:OTTDPO>2.0.CO;2.
   RAMASWAMY C, 1962, TELLUS, V14, P337, DOI 10.1111/j.2153-3490.1962.tb01346.x.
   RASMUSSON EM, 1982, MON WEATHER REV, V110, P354, DOI 10.1175/1520-0493(1982)110<0354:VITSST>2.0.CO;2.
   ROPELEWSKI CF, 1987, MON WEATHER REV, V115, P1606, DOI 10.1175/1520-0493(1987)115<1606:GARSPP>2.0.CO;2.
   Shen XH, 1998, J METEOROL SOC JPN, V76, P217, DOI 10.2151/jmsj1965.76.2\_217.
   SHUKLA J, 1983, MON WEATHER REV, V111, P1830, DOI 10.1175/1520-0493(1983)111<1830:TSOALR>2.0.CO;2.
   SHUKLA J, 198

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