text:
J CLIMATE, V10, P1004, DOI 10.1175/1520-0442(1997)010<1004:ELIV>2.0.CO;2.}},
Number-of-Cited-References = {{55}},
Times-Cited = {{11}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{9}},
Journal-ISO = {{Holocene}},
Doc-Delivery-Number = {{822FT}},
Unique-ID = {{ISI:000221524900011}},
DA = {{2020-08-06}},
}

@article{ ISI:000221195200001,
Author = {Huang, F and Zhou, FX and England, MH},
Title = {{Atmospheric circulation associated with anomalous variations in North
   Pacific wintertime blocking}},
Journal = {{MONTHLY WEATHER REVIEW}},
Year = {{2004}},
Volume = {{132}},
Number = {{5}},
Pages = {{1049-1064}},
Month = {{MAY}},
Abstract = {{Atmospheric circulation associated with anomalous variation of North
   Pacific blocking during the northern winter ( December to February) is
   described and examined using the National Centers for Environmental
   Prediction-National Center for Atmospheric Research (NCEP-NCAR)
   reanalysis data from 1948/49 to 1999/2000. The divergent wind and
   pressure vertical velocity are employed for the identification of
   atmospheric circulation cells. There are several atmospheric cells over
   the North Pacific associated with an anomalous blocking situation during
   winter. They are the zonal Walker cell along the equator (ZWC), the
   regional Hadley cell in the western Pacific (WHC), the regional Hadley
   cell in the eastern Pacific (EHC), the regional Ferrel cell over the
   eastern Pacific in the midlatitudes (EFC), and the midlatitude zonal
   cell (MZC) over the Pacific. During a strong blocking winter (SBW), the
   ZWC is strengthened and the anomalous EHC is opposite to the anomalous
   WHC and the thermally driven Hadley cell. The anomalous MZC is
   characterized by air rising in the west part of the North Pacific,
   flowing eastward in the upper troposphere, descending in the eastern
   North Pacific, then returning back to the east coast of Asia in the
   lower troposphere, modulating the mean MZC. It is also found that the
   anomalous regional Ferrel cell at midlatitudes exists in the eastern
   Pacific ( EFC), whereas it is not apparent in the western Pacific. All
   anomalous atmospheric cells almost completely reverse during a weak
   blocking winter (WBW). Evolutions of each cell are also investigated.
   The atmospheric cells over the tropical and subtropical regions ( ZWC,
   EHC, and WHC) always emerge ahead of the anomalous blocking winter, and
   then lower troposphere signals propagate upward after the anomalous
   blocking winter. This may suggest a mid-to-low-latitude interaction of
   the response of the midlatitude atmospheric blocking to tropical SST
   variations and a feedback via the atmospheric cells to the Tropics. In
   contrast, the midlatitude cells ( MZC, EFC) evolve very locally, with a
   simultaneous response to the blocking event and no propagation of
   signal.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Huang, F (Corresponding Author), Ocean Univ China, Dept Marine Meteorol, Lab Phys Oceanog, 5 Yushan Rd, Qingdao 266003, Peoples R China.
   Ocean Univ China, Dept Marine Meteorol, Lab Phys Oceanog, Qingdao 266003, Peoples R China.
   Univ New S Wales, Sydney, NSW, Australia.}},
DOI = {{10.1175/1520-0493(2004)132<1049:ACAWAV>2.0.CO;2}},
ISSN = {{0027-0644}},
EISSN = {{1520-0493}},
Keywords-Plus = {{DATA ASSIMILATION ANALYSIS; SEA-SURFACE TEMPERATURE; EAST-WEST
   CIRCULATIONS; UPPER OCEAN 1950-95; SOUTHERN OSCILLATION; PERSISTENT
   ANOMALIES; EL-NINO; HEMISPHERE; TELECONNECTION; PROPAGATION}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{huangf@mail.ouc.edu.cn}},
ResearcherID-Numbers = {{England, Matthew H/A-7539-2011}},
ORCID-Numbers = {{England, Matthew H/0000-0001-9696-2930}},
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Number-of-Cited-References = {{39}},
Times-Cited = {{8}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{4}},
Journal-ISO = {{Mon. Weather Rev.}},
Doc-Delivery-Number = {{817RS}},
Unique-ID = {{ISI:000221195200001}},
DA = {{2020-08-06}},
}

@article{ ISI:000189185900013,
Author = {Ozkan, B and Akcaoz, H and Fert, C},
Title = {{Energy input-output analysis in Turkish agriculture (vol 29, pg 39,
   2004)}},
Journal = {{RENEWABLE ENERGY}},
Year = {{2004}},
Volume = {{29}},
Number = {{6}},
Pages = {{1003}},
Month = {{MAY}},
Publisher = {{PERGAMON-ELSEVIER SCIENCE LTD}},
Address = {{THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND}},
Type = {{Correction}},
Language = {{English}},
Affiliation = {{Ozkan, B (Corresponding Author), Univ Akdeniz, Fac Agr, Dept Agr Econ, TR-07058 Antalya, Turkey.
   Univ Akdeniz, Fac Agr, Dept Agr Econ, TR-07058 Antalya, Turkey.}},
DOI = {{10.1016/j.renene.2003.11.007}},
ISSN = {{0960-1481}},
Research-Areas = {{Science \& Technology - Other Topics; Energy \& Fuels}},
Web-of-Science-Categories  = {{Green \& Sustainable Science \& Technology; Energy \& Fuels}},
ResearcherID-Numbers = {{AKCAOZ, HANDAN/C-2475-2016}},
Cited-References = {{Ozkan B, 2004, RENEW ENERG, V29, P39, DOI 10.1016/S0960-1481(03)00135-6.}},
Number-of-Cited-References = {{1}},
Times-Cited = {{0}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{6}},
Journal-ISO = {{Renew. Energy}},
Doc-Delivery-Number = {{777PC}},
Unique-ID = {{ISI:000189185900013}},
DA = {{2020-08-06}},
}

@article{ ISI:000220944500004,
Author = {Pourmand, A and Marcantonio, F and Schulz, H},
Title = {{Variations in productivity and eolian fluxes in the northeastern Arabian
   Sea during the past 110 ka}},
Journal = {{EARTH AND PLANETARY SCIENCE LETTERS}},
Year = {{2004}},
Volume = {{221}},
Number = {{1-4}},
Pages = {{39-54}},
Month = {{APR 30}},
Abstract = {{High-resolution (one to two samples/ka) radionuclide proxy records from
   core 93KL in the northeastern Arabian Sea provide evidence for
   millennial climate variability over the past 110 ka. We interpret
   Th-230-normalized Th-232 fluxes as a proxy for eolian input, and
   authigenic uranium concentrations as a proxy for past productivity. We
   attribute orbital and suborbital variations in both proxies to changes
   in the intensity of the southwest Indian Ocean monsoon. The highest
   Th-230-normalized Th-232 fluxes occur at times that are consistent with
   the timing of the Younger Dryas, Heinrich events 1-7 and cold
   Dansgaard-Oeschger stadial events recorded in the GISP2 ice core. Such
   high dust fluxes may be due to a weakened southwest monsoon in
   conjunction with strengthened northwesterlies from the Arabian Peninsula
   and Mesopotamia. Authigenic uranium concentrations, on the other hand,
   are highest during warm Dansgaard-Oeschger interstadials when the
   southwest monsoon is intensified relative to the northwesterly winds.
   Our results also indicate that on orbital timescales maximum average
   eolian fluxes coincide with the timing of marine isotopic stage (MIS) 2
   and 4, while minimum fluxes occur during MIS 1, 3 and 5. Although the
   forcing mechanism(s) controlling suborbital variabilities in monsoonal
   intensity is still debated, our findings suggest an atmospheric
   teleconnection between the low-latitude southwest monsoon and North
   Atlantic climate. (C) 2004 Elsevier B.V. All rights reserved.}},
Publisher = {{ELSEVIER}},
Address = {{RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Marcantonio, F (Corresponding Author), Tulane Univ, Dept Earth \& Environm Sci, New Orleans, LA 70118 USA.
   Tulane Univ, Dept Earth \& Environm Sci, New Orleans, LA 70118 USA.
   Univ Tubingen, Inst Geowissensch, D-72076 Tubingen, Germany.}},
DOI = {{10.1016/S0012-821X(04)00109-8}},
ISSN = {{0012-821X}},
EISSN = {{1385-013X}},
Keywords = {{millennial variations; Indian Ocean monsoon; eolian flux; productivity;
   uranium-thorium}},
Keywords-Plus = {{DEEP-SEA; OXYGEN-MINIMUM; MONSOON CLIMATE; NORTH-ATLANTIC;
   PARTICLE-FLUX; EXCESS TH-230; SEDIMENTS; PA-231; OCEAN; HOLOCENE}},
Research-Areas = {{Geochemistry \& Geophysics}},
Web-of-Science-Categories  = {{Geochemistry \& Geophysics}},
Author-Email = {{fmarcan@tulane.edu}},
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Number-of-Cited-References = {{51}},
Times-Cited = {{45}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{15}},
Journal-ISO = {{Earth Planet. Sci. Lett.}},
Doc-Delivery-Number = {{813ZH}},
Unique-ID = {{ISI:000220944500004}},
DA = {{2020-08-06}},
}

@article{ ISI:000221346800007,
Author = {Suh, S},
Title = {{Functions, commodities and environmental impacts in an
   ecological-economic model}},
Journal = {{ECOLOGICAL ECONOMICS}},
Year = {{2004}},
Volume = {{48}},
Number = {{4}},
Pages = {{451-467}},
Month = {{APR 20}},
Abstract = {{In contrast to macroscopic tools, life cycle assessment (LCA) starts
   from the microstructure of an economic system: the production and
   consumption of functional flows. Due to the level of resolution required
   for function-level details, the model used for LCA has relied on
   process-specific data and has treated the product system as a
   stand-alone system instead of a system embedded within a broader
   economic system. This separation causes various problems, including
   incompleteness of the system and loss of applicability for a variety of
   analytical tools developed for LCA or economic models. This study aims
   to link the functional flow-based, micro-level LCA system to its
   embedding, commodity-based, meso- or macro-level economic system
   represented by input-output accounts, resulting in a comprehensive
   ecological-economic model within a consistent and flexible mathematical
   framework. For this purpose, the LCA computational structure is
   reformulated into a functional flow by process framework and
   reintroduced in the context of the input-output tradition. It is argued
   that the model presented here overcomes the problem of incompleteness of
   the system and enables various analytical tools developed for LCA or
   input-output analysis (IOA) to be utilised for further analysis. The
   applicability of the model for cleaner production and supply chain
   management is demonstrated using a simplified product system and
   structural path analysis as an example. (C) 2004 Elsevier B.V. All
   rights reserved.}},
Publisher = {{ELSEVIER SCIENCE BV}},
Address = {{PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Suh, S (Corresponding Author), Leiden Univ, Inst Environm Sci, CML, POB 9518, NL-2300 RA Leiden, Netherlands.
   Leiden Univ, Inst Environm Sci, CML, NL-2300 RA Leiden, Netherlands.}},
DOI = {{10.1016/j.ecolecon.2003.10.013}},
ISSN = {{0921-8009}},
Keywords = {{life cycle assessment (LCA); input-output analysis (IOA); hybrid
   analysis; system boundary; comprehensive ecological-economic model;
   functional flow}},
Keywords-Plus = {{INPUT-OUTPUT-ANALYSIS; ALTERNATIVE TREATMENT; SECONDARY PRODUCTS;
   INVENTORIES; FRAMEWORK; CHOICE}},
Research-Areas = {{Environmental Sciences \& Ecology; Business \& Economics}},
Web-of-Science-Categories  = {{Ecology; Economics; Environmental Sciences; Environmental Studies}},
Author-Email = {{suh@cml.leidenuniv.nl}},
ResearcherID-Numbers = {{Suh, Sangwon/E-2019-2011}},
ORCID-Numbers = {{Suh, Sangwon/0000-0001-8290-6276}},
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Number-of-Cited-References = {{53}},
Times-Cited = {{187}},
Usage-Count-Last-180-days = {{2}},
Usage-Count-Since-2013 = {{61}},
Journal-ISO = {{Ecol. Econ.}},
Doc-Delivery-Number = {{819WM}},
Unique-ID = {{ISI:000221346800007}},
DA = {{2020-08-06}},
}

@article{ ISI:000222354600011,
Author = {Haddad, EA},
Title = {{Input-output analysis: Frontiers and extensions}},
Journal = {{PAPERS IN REGIONAL SCIENCE}},
Year = {{2004}},
Volume = {{83}},
Number = {{2}},
Pages = {{510-512}},
Month = {{APR}},
Publisher = {{SPRINGER}},
Address = {{233 SPRING STREET, NEW YORK, NY 10013 USA}},
Type = {{Book Review}},
Language = {{English}},
Affiliation = {{Haddad, EA (Corresponding Author), Univ Sao Paulo, Dept Econ, Sao Paulo, Brazil.
   Univ Sao Paulo, Dept Econ, Sao Paulo, Brazil.}},
ISSN = {{1056-8190}},
Research-Areas = {{Business \& Economics; Environmental Sciences \& Ecology; Geography;
   Public Administration}},
Web-of-Science-Categories  = {{Economics; Environmental Studies; Geography; Regional \& Urban Planning}},
ResearcherID-Numbers = {{Haddad, Eduardo/H-2762-2012}},
ORCID-Numbers = {{Haddad, Eduardo/0000-0001-6564-6716}},
Cited-References = {{Lahr M.L., 2001, INPUT OUTPUT ANAL FR.}},
Number-of-Cited-References = {{1}},
Times-Cited = {{0}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{1}},
Journal-ISO = {{Pap. Reg. Sci.}},
Doc-Delivery-Number = {{833QY}},
Unique-ID = {{ISI:000222354600011}},
DA = {{2020-08-06}},
}

@article{ ISI:000222369600001,
Author = {Forchhammer, MC and Post, E},
Title = {{Using large-scale climate indices in climate change ecology studies}},
Journal = {{POPULATION ECOLOGY}},
Year = {{2004}},
Volume = {{46}},
Number = {{1}},
Pages = {{1-12}},
Month = {{APR}},
Abstract = {{Recently, climate change research in ecology has embraced the use of
   large-scale climate indices in long-term, retrospective studies. In most
   instances, these indices are related to large-scale teleconnection and
   atmospheric patterns of which over a dozen have been identified.
   Although most of these relate to different geographical areas, many are
   related and interact. Consequently, even the simple task of selecting
   one to use in ecological research has become complicated, despite our
   ability to disentangle the results from analyses involving large-scale
   climate indices. Leaning upon recent reviews of the definition and
   functioning of large-scale climate indices, as well as reviews on the
   relationship between these and concomitant changes in ecological
   variables, we focus here on the usefulness of large-scale climate
   indices in different aspects of climate change ecology. By providing a
   general framework for using climate indices, we illustrate the potential
   advantages of their utility by integrating three case histories focusing
   on two groups of evolutionarily distinct organisms: birds and mammals.}},
Publisher = {{WILEY}},
Address = {{111 RIVER ST, HOBOKEN 07030-5774, NJ USA}},
Type = {{Review}},
Language = {{English}},
Affiliation = {{Forchhammer, MC (Corresponding Author), Univ Copenhagen, Inst Biol, Dept Populat Biol, Univ Pk 15, DK-2100 Copenhagen, Denmark.
   Univ Copenhagen, Inst Biol, Dept Populat Biol, DK-2100 Copenhagen, Denmark.
   Penn State Univ, Dept Biol, University Pk, PA 16802 USA.}},
DOI = {{10.1007/s10144-004-0176-x}},
ISSN = {{1438-3896}},
EISSN = {{1438-390X}},
Keywords = {{ecological responses; El Nino 3.4; longterm climate variability; North
   Atlantic Oscillation; North Pacific Oscillation; teleconnection patterns}},
Keywords-Plus = {{NORTH-ATLANTIC OSCILLATION; VOLE CLETHRIONOMYS RUFOCANUS; SEX-RATIO
   VARIATION; POPULATION-DYNAMICS; RED DEER; EXTRINSIC MODIFICATION;
   DENSITY-DEPENDENCE; LONG-DISTANCE; VARIABILITY; PHENOLOGY}},
Research-Areas = {{Environmental Sciences \& Ecology}},
Web-of-Science-Categories  = {{Ecology}},
Author-Email = {{mcforchhammer@bi.ku.dk}},
ResearcherID-Numbers = {{Forchhammer, Mads/I-7474-2013}},
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Number-of-Cited-References = {{66}},
Times-Cited = {{63}},
Usage-Count-Last-180-days = {{2}},
Usage-Count-Since-2013 = {{37}},
Journal-ISO = {{Popul. Ecol.}},
Doc-Delivery-Number = {{833VW}},
Unique-ID = {{ISI:000222369600001}},
DA = {{2020-08-06}},
}

@article{ ISI:000220393800011,
Author = {Sarkar, S and Kafatos, M},
Title = {{Interannual variability of vegetation over the Indian sub-continent and
   its relation to the different meteorological parameters}},
Journal = {{REMOTE SENSING OF ENVIRONMENT}},
Year = {{2004}},
Volume = {{90}},
Number = {{2}},
Pages = {{268-280}},
Month = {{MAR 30}},
Abstract = {{The dynamic nature of climate over Indian sub-continent is well known
   which influences Indian monsoon. Such dynamic variability of climate
   factors can also have significant implications for the vegetation and
   agricultural productivity of this region. Using empirical orthogonal
   function (EOF) and wavelet decomposition techniques, normalized
   difference vegetation index (NDVI) monthly data over Indian
   sub-continent for 18 years from 1982 to 2000 have been used to study the
   variability of vegetation. The present study shows that the monsoon
   precipitation and land surface temperature over the Indian sub-continent
   landmass have significant impact on the distribution of vegetation.
   Tropospheric aerosols exert a strong influence too, albeit secondary to
   monsoon precipitation and prove to be a powerful governing factor. Local
   climate anomaly is seen to be more effective in determining the
   vegetation change than any global teleconnection effects. The study
   documents the dominating influence of monsoon precipitation and
   highlights the importance of aerosols on the vegetation and necessitates
   the need for remedial measures. The present study and an earlier one
   point towards a possible global teleconnection pattern of ENSO as it is
   seen to affect a particular mode of vegetation worldwide. (C) 2004
   Elsevier Inc. All rights reserved.}},
Publisher = {{ELSEVIER SCIENCE INC}},
Address = {{360 PARK AVE SOUTH, NEW YORK, NY 10010-1710 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Sarkar, S (Corresponding Author), George Mason Univ, Sch Computat Sci, Ctr Earth Observing \& Space Res, MS 5C3,4400 Univ Dr, Fairfax, VA 22030 USA.
   George Mason Univ, Sch Computat Sci, Ctr Earth Observing \& Space Res, Fairfax, VA 22030 USA.}},
DOI = {{10.1016/j.rse.2004.01.003}},
ISSN = {{0034-4257}},
EISSN = {{1879-0704}},
Keywords = {{interannual variability; vegetation over; Indian sub-continent}},
Keywords-Plus = {{SEA-SURFACE TEMPERATURE; NINO SOUTHERN-OSCILLATION; TIBETAN PLATEAU;
   SATELLITE DATA; UNITED-STATES; MONSOON; INDEX; ENSO; EVOLUTION;
   EXTENSION}},
Research-Areas = {{Environmental Sciences \& Ecology; Remote Sensing; Imaging Science \&
   Photographic Technology}},
Web-of-Science-Categories  = {{Environmental Sciences; Remote Sensing; Imaging Science \& Photographic
   Technology}},
Author-Email = {{ssarkar@gmu.edu}},
ResearcherID-Numbers = {{Sarkar, Sudipta/I-5545-2019}},
ORCID-Numbers = {{Sarkar, Sudipta/0000-0003-0551-6543}},
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Number-of-Cited-References = {{39}},
Times-Cited = {{73}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{21}},
Journal-ISO = {{Remote Sens. Environ.}},
Doc-Delivery-Number = {{805VM}},
Unique-ID = {{ISI:000220393800011}},
DA = {{2020-08-06}},
}

@article{ ISI:000220442000002,
Author = {Coulibaly, P and Burn, DH},
Title = {{Wavelet analysis of variability in annual Canadian streamflows}},
Journal = {{WATER RESOURCES RESEARCH}},
Year = {{2004}},
Volume = {{40}},
Number = {{3}},
Month = {{MAR 16}},
Abstract = {{Wavelet analysis is used to identify and describe variability in annual
   Canadian streamflows and to gain insights into the dynamical link
   between the streamflows and the dominant modes of climate variability in
   the Northern Hemisphere. Results from applying continuous wavelet
   transform to mean annual streamflows from 79 rivers selected from the
   Canadian Reference Hydrometric Basin Network (RHBN) reveal striking
   climate-related features before the 1950s and after the 1970s. The span
   of available observations, 1911-1999, allows for depicting variance for
   periods up to 12 years. Scale-averaged wavelet power spectra are used to
   simultaneously assess the interannual and spatial variability in 79
   annual streamflow time series. The most striking feature, in the 2-3
   year band and in the 3-6 year band (the 6-12 year band is dominated by
   white noise ( since 1950) and is not considered further) is a net
   distinction between the timing and intensity of the interannual
   variability in western, central, and eastern streamflows, which is shown
   to be linked to the regional climatology. It is found that for the 2-3
   year band, the Canadian streamflows are depicted mainly by the Pacific
   North America (PNA) during 1950-1999, and the Northern Hemisphere
   Annular Mode (NAM) only prior to 1950, and the North Atlantic
   Oscillation (NAO) after 1970. Similarly, in the 3-6 year band, the
   streamflows are depicted mostly by the NAO, the sea surface temperature
   anomalies over the Nino-3 region (ENSO3) and the PNA during the period
   1950-1999, and the NAM prior to 1950. Furthermore, strong local
   correlations between teleconnection patterns and western, central, and
   eastern streamflows are also revealed in both the 2-3 and 3-6 year bands
   with striking changes around 1950 and 1970. The correlation analysis in
   the 2-3 year and 3-6 year bands revealed the presence of two change
   points in the west and east streamflows occurring around 1950 and 1970.}},
Publisher = {{AMER GEOPHYSICAL UNION}},
Address = {{2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Coulibaly, P (Corresponding Author), McMaster Univ, Dept Civil Engn, Hamilton, ON L8S 4L7, Canada.
   McMaster Univ, Dept Civil Engn, Hamilton, ON L8S 4L7, Canada.
   McMaster Univ, Sch Geog \& Geol, Hamilton, ON L8S 4L7, Canada.
   Univ Waterloo, Dept Civil Engn, Waterloo, ON N2L 3G1, Canada.}},
DOI = {{10.1029/2003WR002667}},
Article-Number = {{W03105}},
ISSN = {{0043-1397}},
Keywords = {{streamflows; wavelet analysis; space-time variability; climatic
   patterns; change point}},
Keywords-Plus = {{NORTH-ATLANTIC OSCILLATION; NINO-SOUTHERN-OSCILLATION; ATMOSPHERIC
   CIRCULATION PATTERNS; UNITED-STATES STREAMFLOW; SEA-SURFACE TEMPERATURE;
   EL-NINO; INTERANNUAL VARIABILITY; GEOPOTENTIAL HEIGHT; ARCTIC
   OSCILLATION; TIME-SERIES}},
Research-Areas = {{Environmental Sciences \& Ecology; Marine \& Freshwater Biology; Water
   Resources}},
Web-of-Science-Categories  = {{Environmental Sciences; Limnology; Water Resources}},
Author-Email = {{couliba@mcmaster.ca
   dhburn@uwaterloo.ca}},
ResearcherID-Numbers = {{Burn, Donald/A-5434-2008
   Burn, Donald/P-7038-2019}},
ORCID-Numbers = {{Burn, Donald/0000-0001-7917-6380}},
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Number-of-Cited-References = {{54}},
Times-Cited = {{151}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{19}},
Journal-ISO = {{Water Resour. Res.}},
Doc-Delivery-Number = {{806OA}},
Unique-ID = {{ISI:000220442000002}},
DA = {{2020-08-06}},
}

@article{ ISI:000220278200006,
Author = {Nieto, S and Frias, MD and Rodriguez-Puebla, C},
Title = {{Assessing two different climatic models and the NCEP-NCAR reanalysis
   data for the description of winter precipitation in the Iberian
   Peninsula}},
Journal = {{INTERNATIONAL JOURNAL OF CLIMATOLOGY}},
Year = {{2004}},
Volume = {{24}},
Number = {{3}},
Pages = {{361-376}},
Month = {{MAR 15}},
Abstract = {{The main questions motivating this study are: Can climate simulations
   describe the observations? To what extent can we use climate models to
   predict climate change? For this purpose, an analysis was made of the
   correspondences and/or discrepancies between observed winter
   precipitation data and the data from the National Centers for
   Environmental Prediction-National Center for Atmospheric Research
   (NCEP-NCAR) reanalysis project, and from two global climatic models:
   ECHAM4/OPYC3 and HadCM3. The data used correspond to the accumulated
   winter precipitation for the period 1949-2000, and comparisons of the
   mean and variability patterns were made. The methods used were principal
   components analysis, to break down variability and reduce the dimensions
   of the fields, and correlation and cross-spectrum analyses for
   comparison of the time series. For all these, we studied the suitability
   of their average distributions, as well as their modes of spatial and
   spectral variability. The results for the Iberian Peninsula show good
   agreement between the precipitation data of the NCEP-NCAR reanalysis and
   the observations, both in the average analysis and in the main modes of
   spatial and time variability. Therefore, the reanalysis data were proved
   to be a good resource for interpreting climate variations. As regards
   the climatic models considered, in general the results point to their
   suitability for describing the spatial distribution of winter
   precipitation, whereas the spectral association is less appropriate. The
   variability of the precipitation data was related to circulation
   patterns and teleconnection indices, such as the North Atlantic
   oscillation and the Arctic oscillation. The results allow us to conclude
   that the discrepancies between the two models and observations must be
   due to a weak representation of the interannual variability. Copyright
   (C) 2004 Royal Meteorological Society.}},
Publisher = {{WILEY}},
Address = {{111 RIVER ST, HOBOKEN 07030-5774, NJ USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Rodriguez-Puebla, C (Corresponding Author), Univ Salamanca, Fac Ciencias, Dept Fis Atmosfera, Plaza Merced S-N, E-37008 Salamanca, Spain.
   Univ Salamanca, Dept Appl Math, Salamanca, Spain.
   Univ Salamanca, Dept Atmospher Phys, Salamanca, Spain.}},
DOI = {{10.1002/joc.999}},
ISSN = {{0899-8418}},
EISSN = {{1097-0088}},
Keywords = {{precipitation variability; climatic models; circulation patterns;
   principal component analysis; spectral analysis; Iberian winter
   precipitation}},
Keywords-Plus = {{CENTER COUPLED MODEL; REGIONAL SCALES; PART I; VARIABILITY; RAINFALL;
   CIRCULATION; PATTERNS; VERSION; TRENDS; LINKS}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{concha@usal.es}},
ResearcherID-Numbers = {{Frias, Maria Dolores MD/F-4874-2012
   Nieto-Isidro, Susana/H-3155-2015
   Rodriguez-Puebla, Concepcion/C-1414-2011}},
ORCID-Numbers = {{Nieto-Isidro, Susana/0000-0002-6751-9398
   Rodriguez-Puebla, Concepcion/0000-0003-0018-6805}},
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Number-of-Cited-References = {{36}},
Times-Cited = {{18}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{2}},
Journal-ISO = {{Int. J. Climatol.}},
Doc-Delivery-Number = {{804DA}},
Unique-ID = {{ISI:000220278200006}},
DA = {{2020-08-06}},
}

@article{ ISI:000189256900017,
Author = {Frey, J and Frey, T and Pajuste, K},
Title = {{Input-output analysis of macroelements in ICP-IM catchment area, Estonia}},
Journal = {{LANDSCAPE AND URBAN PLANNING}},
Year = {{2004}},
Volume = {{67}},
Number = {{1-4}},
Pages = {{217-223}},
Month = {{MAR 15}},
Note = {{IALE European Conference, Stockholm, SWEDEN, 2001}},
Organization = {{IALE}},
Abstract = {{Using bulk deposition, throughfall, stemflow, soil infiltration, runoff
   water, litterfall data, ion mass budgets were calculated for a catchment
   area and for mature spruce and pine stands on it. The ions considered in
   mass balances were Na+, K+, Cat(2+), Mg2+, SO42-, NO3-, NH4+, HCO3-, and
   H+. Corresponding fluxes for the budgets were calculated as an average
   for 6 years of studies (1995-2000). Annual input-output balances of all
   nutrients were positive at the plot-scale, so that leaching into soil
   water was less than the corresponding deposition load. Deposition of Ca,
   Mg, Na and S into soil by precipitation exceeded input through
   litterfall. A proton budget approach shows that the main soil buffering
   process is retention of sulphate, which clearly exceeds weathering. At
   the catchment-scale, input-output analysis shows essential output of
   cations due to weathering from the soil. A distinct change in
   input-output balance of sulphate during study period was evident. The
   retention of sulphur has been replaced by its release from the catchment
   area. (C) 2003 Elsevier Science B.V. All rights reserved.}},
Publisher = {{ELSEVIER}},
Address = {{RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS}},
Type = {{Article; Proceedings Paper}},
Language = {{English}},
Affiliation = {{Frey, J (Corresponding Author), Univ Tartu, Inst Geog, EE-51014 Tartu, Estonia.
   Univ Tartu, Inst Geog, EE-51014 Tartu, Estonia.
   Estonian Agr Univ, Inst Silviculture, EE-51006 Tartu, Estonia.}},
DOI = {{10.1016/S0169-2046(03)00041-0}},
ISSN = {{0169-2046}},
EISSN = {{1872-6062}},
Keywords = {{conifer; catchment; deposition; runoff; soil water}},
Research-Areas = {{Environmental Sciences \& Ecology; Geography; Physical Geography; Public
   Administration; Urban Studies}},
Web-of-Science-Categories  = {{Ecology; Environmental Studies; Geography; Geography, Physical; Regional
   \& Urban Planning; Urban Studies}},
Author-Email = {{jane.frey@mail.ee}},
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Number-of-Cited-References = {{13}},
Times-Cited = {{4}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{7}},
Journal-ISO = {{Landsc. Urban Plan.}},
Doc-Delivery-Number = {{778TM}},
Unique-ID = {{ISI:000189256900017}},
DA = {{2020-08-06}},
}

@article{ ISI:000220225300001,
Author = {Zveryaev, II},
Title = {{Seasonality in precipitation variability over Europe}},
Journal = {{JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES}},
Year = {{2004}},
Volume = {{109}},
Number = {{D5}},
Month = {{MAR 6}},
Abstract = {{{[}1] A gridded monthly and pentad precipitation for 1979 - 2001 from
   the Climate Prediction Center Merged Analysis of Precipitation ( CMAP)
   data set and terrestrial monthly gauge-based precipitation for 1958 -
   1998 from the Climatic Research Unit, University of East Anglia (CRU),
   data set are used to investigate seasonality in the long- and short-term
   precipitation variability over Europe. Prominent seasonal differences
   are detected both in precipitation climatologies and in characteristics
   of precipitation variability. It is shown that over western Europe the
   summer precipitation climatology and its year-to-year variability (
   expressed by standard deviations) are lower than those of the winter
   precipitation. Major seasonal differences are found over central eastern
   Europe. In this region the summer precipitation climatology and
   magnitudes of its interannual variability exceed respective winter
   characteristics by a factor of 2 - 3.5. Similar relationships are found
   for the summer and winter magnitudes of intraseasonal fluctuations of
   precipitation. The first empirical orthogonal function (EOF) modes of
   both summer and winter seasonal mean precipitation over Europe are
   associated with the North Atlantic Oscillation (NAO). However, they
   explain very different ( 42\% for winter and 25\% for summer) fractions
   of total precipitation variability and form principally different
   spatial patterns. Temporal behavior of the respective principal
   components is also essentially different. The first EOF mode of the
   winter magnitudes of intraseasonal precipitation fluctuations is also
   associated with the NAO. The second EOF mode of the winter precipitation
   is linked to the East Atlantic teleconnection pattern. However, the
   respective mode in the magnitudes of intraseasonal fluctuations was not
   detected. The second EOF mode of the summer precipitation is associated
   with the 500 hPa heights pattern, which is characterized by four anomaly
   centers. Two major centers of opposite polarity are located over western
   Europe and Scandinavia- northeastern European Russia.}},
Publisher = {{AMER GEOPHYSICAL UNION}},
Address = {{2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Zveryaev, II (Corresponding Author), RAS, PP Shirshov Oceanol Inst, 36 Nakhimovsky Ave, Moscow 117851, Russia.
   RAS, PP Shirshov Oceanol Inst, Moscow 117851, Russia.}},
DOI = {{10.1029/2003JD003668}},
Article-Number = {{D05103}},
ISSN = {{2169-897X}},
EISSN = {{2169-8996}},
Keywords = {{precipitation; teleconnections; Europe}},
Keywords-Plus = {{NORTH-ATLANTIC OSCILLATION; SEA-LEVEL PRESSURE; ATMOSPHERIC CIRCULATION;
   SOUTHERN OSCILLATION; GLOBAL PRECIPITATION; SURFACE-TEMPERATURE; CLIMATE
   VARIABILITY; GAUGE OBSERVATIONS; LAND AREAS; PATTERNS}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{igorz@sail.msk.ru}},
ResearcherID-Numbers = {{Zveryaev, Igor/U-9876-2019}},
ORCID-Numbers = {{Zveryaev, Igor/0000-0001-6687-303X}},
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Number-of-Cited-References = {{49}},
Times-Cited = {{47}},
Usage-Count-Last-180-days = {{2}},
Usage-Count-Since-2013 = {{9}},
Journal-ISO = {{J. Geophys. Res.-Atmos.}},
Doc-Delivery-Number = {{803IR}},
Unique-ID = {{ISI:000220225300001}},
DA = {{2020-08-06}},
}

@article{ ISI:000220618900014,
Author = {Liu, YF and Chen, XH},
Title = {{Some results on continuous type conditional input-output equation -
   Fixed point and surjectivity methods}},
Journal = {{APPLIED MATHEMATICS AND MECHANICS-ENGLISH EDITION}},
Year = {{2004}},
Volume = {{25}},
Number = {{3}},
Pages = {{358-366}},
Month = {{MAR}},
Abstract = {{Based on the classical ( matrix type) input-output analysis, a type of
   nonlinear (continuous type) conditional Leontief model, input-output
   equation were introduced, as well as three corresponding questions,
   namely, solvability, continuity and surjectivity, and some fixed point
   and surjectivity methods in nonlinear analysis were used to deal with
   these questions. As a result, the main theorems are obtained, which
   provide some sufficient criterions to solve above questions described by
   the boundary properties of the enterprise's consuming operator.}},
Publisher = {{SHANGHAI UNIV}},
Address = {{149 YANCHANG RD, SHANGHAI 200072, PEOPLES R CHINA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Liu, YF (Corresponding Author), Nanjing Univ Aeronaut \& Astronaut, Dept Math, Nanjing 210016, Peoples R China.
   Nanjing Univ Aeronaut \& Astronaut, Dept Math, Nanjing 210016, Peoples R China.
   Nanjing Univ Post \& Telecommun, Dept Math, Nanjing 210003, Peoples R China.}},
ISSN = {{0253-4827}},
Keywords = {{input-output equation; solvability; continuity; surjectivity; fixed
   point; upper semi-continuous; upper hemi-continuous; nonlinear analysis}},
Research-Areas = {{Mathematics; Mechanics}},
Web-of-Science-Categories  = {{Mathematics, Applied; Mechanics}},
Author-Email = {{yingfanliu@hotmail.com}},
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Number-of-Cited-References = {{16}},
Times-Cited = {{6}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{1}},
Journal-ISO = {{Appl. Math. Mech.-Engl. Ed.}},
Doc-Delivery-Number = {{809EB}},
Unique-ID = {{ISI:000220618900014}},
DA = {{2020-08-06}},
}

@article{ ISI:000220450100001,
Author = {Misra, V},
Title = {{An evaluation of the predictability of austral summer season
   precipitation over South America}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2004}},
Volume = {{17}},
Number = {{6}},
Pages = {{1161-1175}},
Month = {{MAR}},
Abstract = {{In this study predictability of austral summer seasonal precipitation
   over South America is investigated using a 12-yr set of a 3.5-month
   range (seasonal) and a 17-yr range (continuous multiannual) five-member
   ensemble integrations of the Center for Ocean-Land-Atmosphere Studies
   (COLA) atmospheric general circulation model (AGCM). These integrations
   were performed with prescribed observed sea surface temperature (SST);
   therefore, skill attained represents an estimate of the upper bound of
   the skill achievable by COLA AGCM with predicted SST. The seasonal runs
   outperform the multiannual model integrations both in deterministic and
   probabilistic skill. The simulation of the January-February-March (JFM)
   seasonal climatology of precipitation is vastly superior in the seasonal
   runs except over the Nordeste region where the multiannual runs show a
   marginal improvement. The teleconnection of the ensemble mean JFM
   precipitation over tropical South America with global contemporaneous
   observed sea surface temperature in the seasonal runs conforms more
   closely to observations than in the multiannual runs. Both the sets of
   runs clearly beat persistence in predicting the interannual
   precipitation anomalies over the Amazon River basin, Nordeste, South
   Atlantic convergence zone, and subtropical South America. However, both
   types of runs display poorer simulations over subtropical regions than
   the tropical areas of South America. The examination of probabilistic
   skill of precipitation supports the conclusions from deterministic skill
   analysis that the seasonal runs yield superior simulations than the
   multiannual-type runs.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Misra, V (Corresponding Author), Inst Global Environm \& Soc Inc, Ctr Ocean Land Atmosphere Studies, 4041 Powder Mill Rd,Suite 302, Calverton, MD 20705 USA.
   Inst Global Environm \& Soc Inc, Ctr Ocean Land Atmosphere Studies, Calverton, MD 20705 USA.}},
DOI = {{10.1175/1520-0442(2004)017<1161:AEOTPO>2.0.CO;2}},
ISSN = {{0894-8755}},
Keywords-Plus = {{GENERAL-CIRCULATION MODELS; NORTHEAST BRAZIL RAINFALL; TIME FORECAST
   SKILL; SURFACE TEMPERATURE; INTERANNUAL VARIABILITY; CLIMATE; ATLANTIC;
   SIMULATIONS; SENSITIVITY; CONVECTION}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{misra@cola.iges.org}},
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