text:
03, P14451, DOI 10.1029/97JC02719.
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Number-of-Cited-References = {{95}},
Times-Cited = {{370}},
Usage-Count-Last-180-days = {{7}},
Usage-Count-Since-2013 = {{98}},
Journal-ISO = {{J. Clim.}},
Doc-Delivery-Number = {{511GQ}},
Unique-ID = {{ISI:000173256600006}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@inproceedings{ ISI:000189002600045,
Author = {Camuffo, D and Sturaro, G and Benito, G},
Editor = {{Thorndycraft, VR and Benito, G and Barriendos, M and Llasat, MC}},
Title = {{An opposite flood pattern teleconnection between the Tagus (Iberian
   Peninsula) and Tiber (Italy) rivers during the last 1000 years}},
Booktitle = {{PALAEOFLOODS, HISTORICAL DATA AND CLIMATIC VARIABILITY: APPLICATIONS IN
   FLOOD RISK ASSESSMENT}},
Year = {{2002}},
Pages = {{295-300}},
Note = {{PHEFRA International Workshop, BARCELONA, SPAIN, OCT 16-19, 2002}},
Organization = {{Spanish Commiss Sci \& Technol; Gen Catalunya, Dept Environm; Gen
   Catalunya, Dept Interior; CSIC}},
Abstract = {{The Iberian Peninsula and Italy have several geographic similarities.
   However, they respond in a different way to Westerlies, to the
   displacement of the polar front and the jet stream. The precipitation
   regime is determined by different weather situations, which may lead, in
   some acute episodes, to a river overflowing. This paper concerns the
   cross comparison between two long series of river overflowing, the River
   Tagus (Spain and Portugal) and the River Tiber (Italy). The present
   analysis shows that, in the last millennium, the two rivers never
   overflowed simultaneously, or at least within the same month. The
   information derived from documentary proxy evidence concerning flooding
   rivers adds new light to the Little Ice Age in Southern Europe.}},
Publisher = {{CONSEJO SUPERIOR INVESTIGACIONES CIENT, CISC}},
Address = {{SERRANO 115 DPDO, 28006 MADRID, SPAIN}},
Type = {{Proceedings Paper}},
Language = {{English}},
Affiliation = {{Camuffo, D (Corresponding Author), CNR, Inst Atmospher Sci \& Climate, Corso Stati Uniti 4, I-35127 Padua, Italy.
   CNR, Inst Atmospher Sci \& Climate, I-35127 Padua, Italy.}},
ISBN = {{84-921958-2-7}},
Keywords-Plus = {{SOUTHERN SPAIN; TIME SCALES; VARIABILITY; FREQUENCY}},
Research-Areas = {{Environmental Sciences \& Ecology; Geology; History}},
Web-of-Science-Categories  = {{Environmental Sciences; Geosciences, Multidisciplinary; History}},
ResearcherID-Numbers = {{Benito, Gerardo/AAK-4763-2020
   Benito, Gerardo/E-5456-2013
   Camuffo, Dario/AAU-3695-2020}},
ORCID-Numbers = {{Benito, Gerardo/0000-0003-0724-1790
   Benito, Gerardo/0000-0003-0724-1790
   }},
Cited-References = {{BARRIENDOS M, 1996, REV GEOGRAFIA, V30, P69.
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Number-of-Cited-References = {{13}},
Times-Cited = {{9}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{2}},
Doc-Delivery-Number = {{BY35D}},
Unique-ID = {{ISI:000189002600045}},
DA = {{2020-08-06}},
}

@inproceedings{ ISI:000180721200265,
Author = {Wang, GH and Wang, HL},
Editor = {{Lan, H}},
Title = {{Research on the estimation of Zhuanghe new harbor's influence on the
   regional economy}},
Booktitle = {{PROCEEDINGS OF 2002 INTERNATIONAL CONFERENCE ON MANAGEMENT SCIENCE \&
   ENGINEERING, VOLS I AND II}},
Year = {{2002}},
Pages = {{1322-1325}},
Note = {{International Conference on Management Science and Engineering, MOSCOW,
   RUSSIA, OCT 22-24, 2002}},
Organization = {{Moscow State Acad Management; Harbin Inst Technol}},
Abstract = {{This paper estimates the influences on production value of various
   sectors derived from Zhuanghe new harbor based on the input-output
   tables, analyzes the interdependence of economic-technology relations
   among these sectors. The results reveal that the construction of
   Zhuanghe new harbor will have significant influences on its local
   economy..}},
Publisher = {{HARBIN INSTITUTE TECHNOLOGY PUBLISHERS}},
Address = {{16 FUXINGJIE NANGANGQU, HARBIN 150006, HEILONGJIANG, PEOPLES R CHINA}},
Type = {{Proceedings Paper}},
Language = {{English}},
Affiliation = {{Wang, GH (Corresponding Author), Dalian Univ Technol, Sch Management, Dalian 116023, Peoples R China.
   Dalian Univ Technol, Sch Management, Dalian 116023, Peoples R China.}},
ISBN = {{7-5603-1793-6}},
Keywords = {{influence on economy; input-output analysis; estimation}},
Research-Areas = {{Business \& Economics; Computer Science; Operations Research \&
   Management Science}},
Web-of-Science-Categories  = {{Business, Finance; Computer Science, Artificial Intelligence; Computer
   Science, Information Systems; Economics; Operations Research \&
   Management Science}},
Cited-References = {{FURUKAWA S, 1986, INT INPUT OUTPUT ANA, P42.
   OCORNER, 1984, INPUT OUTPUT ANAL AP.
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   1987, CHINA INPUT OUTPUT T.}},
Number-of-Cited-References = {{6}},
Times-Cited = {{0}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{0}},
Doc-Delivery-Number = {{BW04N}},
Unique-ID = {{ISI:000180721200265}},
DA = {{2020-08-06}},
}

@inproceedings{ ISI:000181352300120,
Author = {Bliman, PA},
Book-Group-Author = {{IEEE
   IEEE}},
Title = {{LMIs for delay-independent properties of delay systems and input-output
   analysis of systems with complex parameter}},
Booktitle = {{PROCEEDINGS OF THE 41ST IEEE CONFERENCE ON DECISION AND CONTROL, VOLS
   1-4}},
Series = {{IEEE CONFERENCE ON DECISION AND CONTROL - PROCEEDINGS}},
Year = {{2002}},
Pages = {{650-655}},
Note = {{41st IEEE Conference on Decision and Control, LAS VEGAS, NV, DEC 10-13,
   2002}},
Organization = {{IEEE Control Syst Soc; Soc Ind \& Appl Math; Inst Operat Res \&
   Management Sci}},
Abstract = {{This note focuses on delay-independent input-output properties
   (passivity, H,,, performance, circle criterion, Popov criterion) of
   delay systems. The main results show that, as it is the case for the
   usual, rational, systems, these properties may be characterized by
   solvability of some linear matrix inequalities. The latter are
   constructed by use of some quadratic Lyapunov-Krasovskii functionals,
   generalizing a well-known class. The method also applies to the analysis
   of systems with uncertain complex parameter, for which the results are
   related to the search for polynomial parameter-dependent Lyapunov
   functions. Illustrative examples are provided.}},
Publisher = {{IEEE}},
Address = {{345 E 47TH ST, NEW YORK, NY 10017 USA}},
Type = {{Proceedings Paper}},
Language = {{English}},
Affiliation = {{Bliman, PA (Corresponding Author), INRIA, Rocquencourt BP 105, F-78153 Le Chesnay, France.
   INRIA, F-78153 Le Chesnay, France.}},
ISSN = {{0191-2216}},
ISBN = {{0-7803-7516-5}},
Keywords-Plus = {{STABILITY; EQUATION}},
Research-Areas = {{Automation \& Control Systems; Computer Science; Operations Research \&
   Management Science}},
Web-of-Science-Categories  = {{Automation \& Control Systems; Computer Science, Artificial
   Intelligence; Operations Research \& Management Science}},
ResearcherID-Numbers = {{Bliman, P.-A./H-7007-2014}},
ORCID-Numbers = {{Bliman, P.-A./0000-0002-7734-2928}},
Cited-References = {{Bliman PA, 2002, IEEE T AUTOMAT CONTR, V47, P327, DOI 10.1109/9.983374.
   BLIMAN PA, 2001, 4278 INRIA.
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   KAMEN EW, 1985, MATH APPL, V16, P101.
   KHALIL HK, 1992, NONLINEAR SYSTEMS.}},
Number-of-Cited-References = {{10}},
Times-Cited = {{0}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{0}},
Doc-Delivery-Number = {{BW26E}},
Unique-ID = {{ISI:000181352300120}},
DA = {{2020-08-06}},
}

@inproceedings{ ISI:000181352300413,
Author = {Ito, H},
Book-Group-Author = {{IEEE
   IEEE}},
Title = {{A constructive proof of ISS small-gain theorem using generalized scaling}},
Booktitle = {{PROCEEDINGS OF THE 41ST IEEE CONFERENCE ON DECISION AND CONTROL, VOLS
   1-4}},
Series = {{IEEE CONFERENCE ON DECISION AND CONTROL - PROCEEDINGS}},
Year = {{2002}},
Pages = {{2286-2291}},
Note = {{41st IEEE Conference on Decision and Control, LAS VEGAS, NV, DEC 10-13,
   2002}},
Organization = {{IEEE Control Syst Soc; Soc Ind \& Appl Math; Inst Operat Res \&
   Management Sci}},
Abstract = {{This paper presents a Lyapunov-type proof of the Input-to-State
   Stable(ISS) small-gain theorem. The proof given in this paper
   demonstrates how to construct a Lyapunov function explicitly, which
   contrasts with existing proofs based on input-output analysis. The
   Lyapunov functions are constructed by selecting state-dependent scaling
   functions properly. The construction of Lyapunov functions motivates the
   author to formulate a new criterion for stability and performance of
   interconnected nonlinear systems. Furthermore, an ISS small-gain
   condition with nonlinearly-scaled supply rates is obtained naturally in
   order to reduce the conservatism arising in the application of the ISS
   small-gain condition.}},
Publisher = {{IEEE}},
Address = {{345 E 47TH ST, NEW YORK, NY 10017 USA}},
Type = {{Proceedings Paper}},
Language = {{English}},
Affiliation = {{Ito, H (Corresponding Author), Kyushu Inst Technol, Dept Control Engn \& Sci, 680-4 Kawazu, Iizuka, Fukuoka 8208502, Japan.
   Kyushu Inst Technol, Dept Control Engn \& Sci, Iizuka, Fukuoka 8208502, Japan.}},
ISSN = {{0191-2216}},
ISBN = {{0-7803-7516-5}},
Keywords-Plus = {{SYSTEMS; STABILITY}},
Research-Areas = {{Automation \& Control Systems; Computer Science; Operations Research \&
   Management Science}},
Web-of-Science-Categories  = {{Automation \& Control Systems; Computer Science, Artificial
   Intelligence; Operations Research \& Management Science}},
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Number-of-Cited-References = {{17}},
Times-Cited = {{9}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{0}},
Doc-Delivery-Number = {{BW26E}},
Unique-ID = {{ISI:000181352300413}},
DA = {{2020-08-06}},
}

@article{ ISI:000178308900025,
Author = {Schwing, FB and Murphree, T and deWitt, L and Green, PM},
Title = {{The evolution of oceanic and atmospheric anomalies in the northeast
   Pacific during the El Nino and La Nina events of 1995-2001}},
Journal = {{PROGRESS IN OCEANOGRAPHY}},
Year = {{2002}},
Volume = {{54}},
Number = {{1-4}},
Pages = {{459-491}},
Note = {{Workshop on El Nino Along the West Coast of North America, MOSS LANDING,
   CA, DEC 06-09, 1999}},
Abstract = {{From late 1995 through early 2001, three major interannual climate
   events occurred in the tropical Pacific; the 199597 La Nina (LN),
   1997-98 El Nino (EN), and 1998-2001 LN. We analyze atmospheric and upper
   oceanic anomalies in the northeast Pacific (NEP) during these events,
   and compare them to anomalies both elsewhere in the north and tropical
   Pacific, and to typical EN and LN anomaly patterns. The atmospheric and
   oceanic anomalies varied strongly on intraseasonal and interannual
   scales. During the 1995-97 LN and 1997-98 EN, the Northeast Pacific was
   dominated by negative SLP and cyclonic wind anomalies, and by upper
   ocean temperature and sea surface height (SSH) anomalies. The latter
   were positive along the North American west coast and in the NEP thermal
   anomaly pool (between Hawaii, Vancouver Island, and Baja California),
   and negative in the central north Pacific. This atmospheric/oceanic
   anomaly pattern is typical of EN. An eastward shift in the atmospheric
   teleconnection from east Asia created EN-like anomalies in the NEP
   during the 1995-97 LN, well before the 1997-98 EN had begun. The
   persistence of negative sea-level pressure (SLP) and cyclonic wind
   anomalies in the NEP during the 1997-98 EN intensified pre-existing
   upper oceanic anomalies. Atmospheric anomalies were shifted eastward
   during late 1996-early 1998, leading to a similar onshore shift of
   oceanic anomalies. This produced exceptionally strong positive upper
   ocean temperature and SSH anomalies along the west coast during the
   1997-98 EN, and explains the unusual coastal occurrences of several
   species of large pelagic warm-water fishes. The growth and eastward
   shift of these pre-existing anomalies does not appear to have been
   linked to tropical Pacific EN anomalies until late 1997, when a clear
   atmospheric teleconnection between the two regions developed. Prior to
   this, remote atmospheric impacts on the NEP were primarily from east
   Asia. As the 19982001 LN developed, NEP anomalies began reversing toward
   the typical LN pattern. This led to predominantly negative SLP and
   cyclonic wind anomalies in the NEP, and upper ocean temperature and SSH
   anomalies that were mainly negative along the west coast and positive in
   the central north Pacific. The persistence of these anomalies into
   mid-2001, and a number of concurrent biological changes in the NEP,
   suggest that a decadal climate shift may have occurred in late 1998.
   During 1995-2001, NEP oceanic anomalies tracked the overlying
   atmospheric anomalies, as indicated by the maintenance of a
   characteristic spatial relationship between these anomalies. In
   particular, wind stress curl and SSH anomalies in the NEP maintained an
   inverse relationship that strengthened and shifted eastward toward the
   west coast during late 1996-early 1998. This consistent relationship
   indicates that anomalous Ekman transport driven by regional atmospheric
   forcing was an important contributor to temperature and SSH anomalies in
   the NEP and CCS during the 1997-98 EN. Other studies have shown that
   coastal propagations originating from the tropical Pacific also may have
   contributed to coastal NEP anomalies during this EN. Our results
   indicate that at least some of this coastal anomaly signal may have been
   generated by regional atmospheric forcing within the NEP. Published by
   Elsevier Science Ltd.}},
Publisher = {{PERGAMON-ELSEVIER SCIENCE LTD}},
Address = {{THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND}},
Type = {{Article; Proceedings Paper}},
Language = {{English}},
Affiliation = {{Schwing, FB (Corresponding Author), NOAA, NMFS, SWFSC, Pacific Fisheries Environm Lab, 1352 Lighthouse Ave, Pacific Grove, CA 93950 USA.
   NOAA, NMFS, SWFSC, Pacific Fisheries Environm Lab, Pacific Grove, CA 93950 USA.
   USN, Postgrad Sch, Dept Meteorol, Monterey, CA 93943 USA.
   Univ Hawaii, Joint Inst Marine \& Atmospher Res, Honolulu, HI 96822 USA.}},
DOI = {{10.1016/S0079-6611(02)00064-2}},
Article-Number = {{PII S0079-6611(02)00064-2}},
ISSN = {{0079-6611}},
Keywords = {{atmospheric circulation; climate; El Nino phenomena; eastern boundary
   currents; upwelling}},
Keywords-Plus = {{CALIFORNIA CURRENT SYSTEM; INTERANNUAL VARIABILITY;
   SOUTHERN-OSCILLATION; WEST-COAST; SEA-LEVEL; CLIMATE OSCILLATIONS;
   EQUATORIAL PACIFIC; REGIME SHIFTS; WIND STRESS; HEAT-FLUX}},
Research-Areas = {{Oceanography}},
Web-of-Science-Categories  = {{Oceanography}},
Author-Email = {{fschwing@pfeg.noaa.gov}},
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Number-of-Cited-References = {{64}},
Times-Cited = {{127}},
Usage-Count-Last-180-days = {{2}},
Usage-Count-Since-2013 = {{20}},
Journal-ISO = {{Prog. Oceanogr.}},
Doc-Delivery-Number = {{598ZZ}},
Unique-ID = {{ISI:000178308900025}},
DA = {{2020-08-06}},
}

@article{ ISI:000173910100004,
Author = {Lu, RY and Oh, JH and Kim, BJ},
Title = {{A teleconnection pattern in upper-level meridional wind over the North
   African and Eurasian continent in summer}},
Journal = {{TELLUS SERIES A-DYNAMIC METEOROLOGY AND OCEANOGRAPHY}},
Year = {{2002}},
Volume = {{54}},
Number = {{1}},
Pages = {{44-55}},
Month = {{JAN}},
Abstract = {{One-point correlation analysis on upper-level meridional wind identified
   the existence of a teleconnection pattern in July, which emerges from
   North Africa to East Asia along the westerly jet in the middle
   latitudes. We examined the spatial and temporal structures of this
   teleconnection pattern, and found the unique characteristics rather
   different from the patterns in other elements such as geopotential
   height, streamfunction and vorticity. We also investigated the
   relationship between this teleconnection and precipitation, and
   suggested that the teleconncction is a possible linkage of the EASM to
   the Indian monsoon, and even to subtropical heating anomalies over
   Atlantic.}},
Publisher = {{BLACKWELL MUNKSGAARD}},
Address = {{35 NORRE SOGADE, PO BOX 2148, DK-1016 COPENHAGEN, DENMARK}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Lu, RY (Corresponding Author), Chinese Acad Sci, Inst Atmospher Phys, POB 2718, Beijing 100080, Peoples R China.
   Chinese Acad Sci, Inst Atmospher Phys, Beijing 100080, Peoples R China.
   Korea Meteorol Adm, Meteorol Res Inst, Seoul, South Korea.}},
DOI = {{10.1034/j.1600-0870.2002.00248.x}},
ISSN = {{0280-6495}},
Keywords-Plus = {{500-MB HEIGHT FLUCTUATIONS; ROSSBY-WAVE PROPAGATION; SHORT-TIME SCALES;
   MONSOON RAINFALL; WINTER; LONG; INTERMEDIATE}},
Research-Areas = {{Meteorology \& Atmospheric Sciences; Oceanography}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences; Oceanography}},
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Number-of-Cited-References = {{15}},
Times-Cited = {{148}},
Usage-Count-Last-180-days = {{2}},
Usage-Count-Since-2013 = {{33}},
Journal-ISO = {{Tellus Ser. A-Dyn. Meteorol. Oceanol.}},
Doc-Delivery-Number = {{522RE}},
Unique-ID = {{ISI:000173910100004}},
DA = {{2020-08-06}},
}

@article{ ISI:000175989800001,
Author = {Gong, DY and Ho, CH},
Title = {{The Siberian High and climate change over middle to high latitude Asia}},
Journal = {{THEORETICAL AND APPLIED CLIMATOLOGY}},
Year = {{2002}},
Volume = {{72}},
Number = {{1-2}},
Pages = {{1-9}},
Abstract = {{The Siberian High is the most important atmospheric centre of action in
   Eurasia during the winter months. Here its variability and relationship
   with temperature and precipitation is investigated for the period 1922
   to 2000. The pronounced weakening of the Siberian High during the last
   similar to 20 years is its most remarkable feature. Mean temperature,
   averaged over middle to high latitude Asia (30degrees E- 140degrees E,
   30degrees N-70degrees N), is correlated with the Siberian High central
   intensity (SHCI) with correlation coefficient of -0.58 (1922-1999), and
   for precipitation, the correlation coefficient is - 0.44 (1922-1998).
   Taking the Arctic Oscillation (AO), the SHCI, the Eurasian
   teleconnection pattern (EU), and the Southern Oscillation (SO) index
   into account, 72 percent of the variance in temperature can be explained
   for the period 1949-1997 (for precipitation the variance is 26 percent),
   with the AO alone explaining 30 percent of the variance, and the
   Siberian High contributing 24 percent. The precipitation variance
   explained by the Siberian High is only 9.8 percent of the total.}},
Publisher = {{SPRINGER-VERLAG WIEN}},
Address = {{SACHSENPLATZ 4-6, PO BOX 89, A-1201 VIENNA, AUSTRIA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Gong, DY (Corresponding Author), Beijing Normal Univ, Inst Resources Sci, Key Lab Environm Change \& Nat Disaster, Beijing 100875, Peoples R China.
   Beijing Normal Univ, Inst Resources Sci, Key Lab Environm Change \& Nat Disaster, Beijing 100875, Peoples R China.
   Seoul Natl Univ, Sch Earth \& Environm Sci, Seoul 151742, South Korea.}},
DOI = {{10.1007/s007040200008}},
ISSN = {{0177-798X}},
Keywords-Plus = {{NORTH-ATLANTIC OSCILLATION; EXTRATROPICAL CIRCULATION; WINTER MONSOON;
   TEMPERATURE-VARIATIONS; GEOPOTENTIAL HEIGHT; ARCTIC OSCILLATION; ANNULAR
   MODES; TELECONNECTIONS; PRECIPITATION; VARIABILITY}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
ResearcherID-Numbers = {{Ho, Chang-Hoi/H-8354-2015}},
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Number-of-Cited-References = {{32}},
Times-Cited = {{194}},
Usage-Count-Last-180-days = {{4}},
Usage-Count-Since-2013 = {{50}},
Journal-ISO = {{Theor. Appl. Climatol.}},
Doc-Delivery-Number = {{558WK}},
Unique-ID = {{ISI:000175989800001}},
DA = {{2020-08-06}},
}

@article{ ISI:000178126400005,
Author = {Kutiel, H and Maheras, P and Turkes, M and Paz, S},
Title = {{North Sea Caspian Pattern (NCP) - an upper level atmospheric
   teleconnection affecting the eastern Mediterranean - implications on the
   regional climate}},
Journal = {{THEORETICAL AND APPLIED CLIMATOLOGY}},
Year = {{2002}},
Volume = {{72}},
Number = {{3-4}},
Pages = {{173-192}},
Abstract = {{A calendar of the negative and positive phases of the North Sea -
   Caspian Pattern (NCP) for the period 1958-1998 was used to analyse the
   implication of the NCP upper level teleconnections on the regional
   climate of the eastern Mediterranean basin. Series of monthly mean air
   temperature and monthly total rainfall from 33 stations across Greece,
   Turkey and Israel, for the same period, were used. For each month, from
   October to April, averages of the monthly mean temperatures and the
   monthly rainfall totals as well as the standardized values of both
   parameters were calculated separately for the negative (NCP and the
   positive (NCP (+)) phases of the NCP.
   At all stations and in all months, temperature values were significantly
   higher during the NCP (-) as compared with the NCP (+). Furthermore,
   apart from very few exceptions, the absolute monthly mean maximum and
   monthly mean minimum values were obtained during the NCP (-) and the NCP
   (+) phases, respectively. The maximum impact of the NCP on mean air
   temperature was detected in the continental Anatolian Plateau, where the
   mean seasonal differences are around 3.5degreesC. This influence
   decreases westwards and southwards.
   The influence on the rainfall regime is more complex. Regions exposed to
   the southern maritime trajectories, in Greece and in Turkey, receive
   more rainfall during the NCP (-) phase, whereas in the regions exposed
   to the northern maritime trajectories, such as Crete in Greece, the
   Black Sea region in Turkey, and in all regions of Israel, there is more
   rainfall during the NCP (+) phase. The accumulated rainfall differences
   between the two phases are over 50\% of the seasonal average for some
   stations.
   A comparison of the capabilities of the NCP, the North Atlantic
   Oscillation (NAO) and the Southern Oscillation (SO) indices to
   differentiate between below and above normal temperatures was made. The
   results have placed the NCP, as the best by far of all three
   teleconnections in its ability to differentiate between below or above
   normal temperatures and as the main teleconnection affecting the climate
   of the Balkans, the Anatolian Peninsula and the Middle East. These
   results may serve to downscale General Circulation Model (GCM) scenarios
   to a regional scale and provide forecasts regarding eventual temperature
   and/or precipitation changes.}},
Publisher = {{SPRINGER-VERLAG WIEN}},
Address = {{SACHSENPLATZ 4-6, PO BOX 89, A-1201 VIENNA, AUSTRIA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Kutiel, H (Corresponding Author), Univ Haifa, Dept Geog, IL-31905 Haifa, Israel.
   Univ Haifa, Dept Geog, IL-31905 Haifa, Israel.
   Univ Thessaloniki, Dept Meteorol \& Climatol, Thessaloniki, Greece.
   State Meteorol Serv, Dept Res, Ankara, Turkey.}},
DOI = {{10.1007/s00704-002-0674-8}},
ISSN = {{0177-798X}},
Keywords-Plus = {{MONTHLY RAINFALL CONDITIONS; CIRCULATION INDEXES; TEMPERATURE REGIME;
   LAST CENTURY; TURKEY; PRECIPITATION; OSCILLATION; ANOMALIES; ISRAEL;
   EUROPE}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
ORCID-Numbers = {{Kutiel, Haim/0000-0001-7289-3088}},
Cited-References = {{Ben-Gai T, 2001, THEOR APPL CLIMATOL, V69, P171, DOI 10.1007/s007040170023.
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Number-of-Cited-References = {{18}},
Times-Cited = {{94}},
Usage-Count-Last-180-days = {{3}},
Usage-Count-Since-2013 = {{13}},
Journal-ISO = {{Theor. Appl. Climatol.}},
Doc-Delivery-Number = {{595UD}},
Unique-ID = {{ISI:000178126400005}},
DA = {{2020-08-06}},
}

@article{ ISI:000173955800002,
Author = {Kutiel, H and Benaroch, Y},
Title = {{North Sea-Caspian Pattern (NCP) - an upper level atmospheric
   teleconnection affecting the Eastern Mediterranean: Identification and
   definition}},
Journal = {{THEORETICAL AND APPLIED CLIMATOLOGY}},
Year = {{2002}},
Volume = {{71}},
Number = {{1-2}},
Pages = {{17-28}},
Abstract = {{An upper level atmospheric teleconnection between grid points: 0degrees,
   55degrees N; 10degrees E, 55degrees N (North Sea) and 50degrees E,
   45degrees N; 60degreesE, 45degreesN (northern Caspian) was identified.
   This teleconnection, referred as the North Sea-Caspian Pattern (NCP) is
   evident at the 500 hPa level. The NCP is more pronounced during winter
   and the transitional seasons. An index (NCPI) measures the geopotential
   heights differences between the two poles of the NCP. Time series of the
   NCPI are presented and analysed. Except for September, no significant
   temporal trends were found. Negative and positive phases of the NCP
   (NCP(-) and NCP(+), respectively) were defined using standardized
   scores. A classification of all months into NCP(-), NCP(+) or normal
   conditions during the analysis period (1958-1998) was prepared and
   analysed. No significant correlation was found between the NCPI and the
   NAO index. The anomalous circulation during either NCP(-) or NCP(+)
   conditions is defined and its possible impact on the regional climate is
   discussed. Preliminary results show below normal temperatures and above
   normal precipitation in the Balkans and the Middle East during NCP(+),
   and the opposite for NCP(-).}},
Publisher = {{SPRINGER WIEN}},
Address = {{SACHSENPLATZ 4-6, PO BOX 89, A-1201 WIEN, AUSTRIA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Kutiel, H (Corresponding Author), Univ Haifa, Dept Geog, IL-31905 Haifa, Israel.
   Univ Haifa, Dept Geog, IL-31905 Haifa, Israel.
   Israel Meterol Serv, IL-50250 Bet Dagan, Israel.}},
DOI = {{10.1007/s704-002-8205-x}},
ISSN = {{0177-798X}},
EISSN = {{1434-4483}},
Keywords-Plus = {{GEOPOTENTIAL HEIGHT FIELD; ATLANTIC OSCILLATION; RAINFALL CONDITIONS;
   TEMPERATURE REGIME; CIRCULATION; EUROPE; ANOMALIES}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{kutiel@geo.haifa.ac.il
   y-benaroch@yahoo.com}},
ORCID-Numbers = {{Kutiel, Haim/0000-0001-7289-3088}},
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Number-of-Cited-References = {{22}},
Times-Cited = {{120}},
Usage-Count-Last-180-days = {{3}},
Usage-Count-Since-2013 = {{10}},
Journal-ISO = {{Theor. Appl. Climatol.}},
Doc-Delivery-Number = {{523LQ}},
Unique-ID = {{ISI:000173955800002}},
DA = {{2020-08-06}},
}

@article{ ISI:000173479100016,
Author = {Landwehr, JM and Winograd, IJ},
Title = {{Dating the Vostok ice core record by importing the Devils Hole
   chronology}},
Journal = {{JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES}},
Year = {{2001}},
Volume = {{106}},
Number = {{D23}},
Pages = {{31853-31861}},
Month = {{DEC 16}},
Abstract = {{The development of an accurate chronology for the Vostok record
   continues to be an open research question because these invaluable ice
   cores cannot be dated directly. Depth-to-age relationships have been
   developed using many different approaches, but published age estimates
   are inconsistent, even for major paleoclimatic events. We have developed
   a chronology for the Vostok deuterium paleotemperature record using a
   simple and objective algorithm to transfer ages of major paleoclimatic
   events from the radiometrically dated 500,000-year
   delta(18)O-paleotemperature record from Devils Hole, Nevada. The method
   is based only on a strong inference that major shifts in
   paleotemperature recorded at both locations occurred synchronously,
   consistent with an atmospheric teleconnection. The derived depth-to-age
   relationship conforms with the physics of ice compaction, and internally
   produces ages for climatic events 5.4 and 11.24 which are consistent
   with the externally assigned ages that the Vostok team needed to assume
   in order to derive their most recent chronology, GT4. Indeed, the
   resulting V-DH chronology is highly correlated with GT4 because of the
   unexpected correspondence even in the timing of second-order climatic
   events that were not constrained by the algorithm. Furthermore, the
   algorithm developed herein is not specific to this problem; rather, the
   procedure can be used whenever two paleoclimate records are proxies for
   the same physical phenomenon, and paleoclimatic conditions forcing the
   two records can be considered to have occurred contemporaneously. The
   ability of the algorithm to date the East Antarctic Dome Fuji core is
   also demonstrated.}},
Publisher = {{AMER GEOPHYSICAL UNION}},
Address = {{2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Landwehr, JM (Corresponding Author), US Geol Survey, Natl Ctr, MS431, Reston, VA 20192 USA.
   US Geol Survey, Natl Ctr, Reston, VA 20192 USA.}},
DOI = {{10.1029/2001JD900065}},
ISSN = {{2169-897X}},
EISSN = {{2169-8996}},
Keywords-Plus = {{LAST GLACIAL PERIOD; CLIMATE-CHANGE; ANTARCTIC PRECIPITATION; TROPICAL
   PACIFIC; ATMOSPHERIC CO2; CYCLES; ORIGIN; GREENLAND; CALCITE; ISOTOPE}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{mjlandwe@usgs.gov
   ijwinogr@usgs.gov}},
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Number-of-Cited-References = {{60}},
Times-Cited = {{9}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{6}},
Journal-ISO = {{J. Geophys. Res.-Atmos.}},
Doc-Delivery-Number = {{515DA}},
Unique-ID = {{ISI:000173479100016}},
DA = {{2020-08-06}},
}

@article{ ISI:000173099400010,
Author = {Janicot, S and Trzaska, S and Poccard, I},
Title = {{Summer Sahel-ENSO teleconnection and decadal time scale SST variations}},
Journal = {{CLIMATE DYNAMICS}},
Year = {{2001}},
Volume = {{18}},
Number = {{3-4}},
Pages = {{303-320}},
Month = {{DEC}},
Abstract = {{The correlation between Sahel rainfall and El Nino-Southern Oscillation
   (ENSO) in the northern summer has been varying for the last fifty years.
   We propose that the existence of periods of weak or strong relationship
   could result from an interaction with the global decadal scale sea
   surface temperature (SST) background. The main modes of SST variability
   have been extracted through a principal component analysis with Varimax
   rotation. The correlations between a July-September Sahel rainfall index
   and these SST modes have been computed on a 20-year running window
   between 1945 and 1993. The correlations with the inter-annual ENSO-SST
   mode are negative, not significant in the 1960s during the transition
   period from the wet climate phasis to the long-running drought in the
   Sahel, but then were significant since 1976. During the former period,
   the correlations between the Sahel rainfall index and the other SST
   modes (expressing mostly on quasi and multi-decadal scales) are the
   highest, in particular correlations with the tropical Atlantic
   ``dipole{''}. Correlations between Sahel and Guinea Coast rainfall are
   also significantly negative. After 1970, the Sahel-Guinea Coast rainfall
   correlations are no longer significant, and the ENSO-SST mode becomes
   the only one significantly correlated with Sahel rainfall, especially
   due to the impact of warm events. The partial correlations between the
   ENSO-SST mode and the Sahel rainfall index, when the influence of the
   other SST modes are eliminated, are significant over all the 20-year
   running periods between 1945 and 1993, suggesting that this summer
   teleconnection could be modulated by the decadal scale SST background.
   The NCEP/NCAR reanalyses reproduce accurately the interannual
   variability of the atmospheric circulation after 1968. In particular a
   regional West African Monsoon Index (WAMI), combining wind speed
   anomalies at 925 and 200 hPa, is highly correlated with the
   July-September Sahel rainfall index. A warm ENSO event is associated
   both with an eastward mean sea level pressure gradient between the
   eastern tropical Pacific and the tropical Atlantic and with a northward
   pressure gradient along the western coast of West Africa. This pattern
   leads to enhanced trade winds over the tropical Atlantic and to weaker
   moisture advection over West Africa, consistent with a weaker monsoon
   system strength and a weaker Southern Hemisphere Hadley circulation. The
   NCEP/NCAR reanalyses do not reproduce accurately the decadal variability
   of the atmospheric circulation over West Africa because of artifical
   biases. Therefore the impact of the decadal scale pattern of the
   atmospheric circulation has been investigated with atmospheric general
   circulation model (AGCM) sensitivity experiments, by forcing the
   ARP-EGE-Climat model with different combinations of an El Nino-like SST
   pattern with the pattern of the main mode of decadal scale SST
   variability where the hightest weights are located in the Pacific and
   Indian basins. AGCM outputs show that the decadal scale SST variations
   weakly affect Sahel rainfall variability but that they do induce an
   indirect effect on Sahel rainfall by enhancing the impact of the warm
   ENSO phases after 1980, through an increase in the fill-in of the
   monsoon trough and a moisture advection deficit over West Africa.}},
Publisher = {{SPRINGER-VERLAG}},
Address = {{175 FIFTH AVE, NEW YORK, NY 10010 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Janicot, S (Corresponding Author), Ecole Polytech, Meteorol Dynam Lab, Meteo France, F-91128 Palaiseau, France.
   Ecole Polytech, Meteorol Dynam Lab, Meteo France, F-91128 Palaiseau, France.
   Univ Bourgogne, CNRS ESA 5080, Ctr Rech Climatol, Dijon, France.}},
DOI = {{10.1007/s003820100172}},
ISSN = {{0930-7575}},
Keywords-Plus = {{SEA-SURFACE TEMPERATURE; SAHARAN WEATHER ANOMALIES; WEST-AFRICAN
   RAINFALL; TROPICAL NORTH-AFRICA; EL-NINO; INTERDECADAL VARIABILITY;
   ATMOSPHERIC CIRCULATION; SOUTHERN OSCILLATION; ATLANTIC; PACIFIC}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
ResearcherID-Numbers = {{Janicot, Serge/E-8493-2012}},
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Number-of-Cited-References = {{65}},
Times-Cited = {{151}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{26}},
Journal-ISO = {{Clim. Dyn.}},
Doc-Delivery-Number = {{508QE}},
Unique-ID = {{ISI:000173099400010}},
DA = {{2020-08-06}},
}

@article{ ISI:000172155800006,
Author = {Jones, JT and Zimmer, RW},
Title = {{Examining the impact of capital on academic achievement}},
Journal = {{ECONOMICS OF EDUCATION REVIEW}},
Year = {{2001}},
Volume = {{20}},
Number = {{6}},
Pages = {{577-588}},
Month = {{DEC}},
Abstract = {{While a growing body of literature on education production looks at the
   impact school inputs have on academic, achievement, virtually no
   research is examining the impact capital is having on academic
   achievement. In this study, we take an initial step towards that end. By
   using school districts' level of bond indebtedness as a proxy for
   capital, we find evidence that capital stock does affect academic
   achievement. In light of these findings along with the general lack of
   research on capital inputs, we conclude that capital expenditures should
   be given greater attention in future research. (C) 2001 Elsevier Science
   Ltd. All rights reserved.}},
Publisher = {{PERGAMON-ELSEVIER SCIENCE LTD}},
Address = {{THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Zimmer, RW (Corresponding Author), RAND Corp, 1700 Main St, Santa Monica, CA 90407 USA.
   RAND Corp, Santa Monica, CA 90407 USA.
   Georgetown Coll, Business Adm \& Econ Dept, Georgetown, KY 40324 USA.}},
DOI = {{10.1016/S0272-7757(00)00043-1}},
ISSN = {{0272-7757}},
Keywords = {{educational economics; educational finance; input output analysis}},
Keywords-Plus = {{PUBLIC-EDUCATION; TEACHERS; SCHOOLS; MATTER; PRODUCTIVITY; UPDATE}},
Research-Areas = {{Business \& Economics; Education \& Educational Research}},
Web-of-Science-Categories  = {{Economics; Education \& Educational Research}},
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Number-of-Cited-References = {{31}},
Times-Cited = {{25}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{7}},
Journal-ISO = {{Econ. Educ. Rev.}},
Doc-Delivery-Number = {{492EQ}},
Unique-ID = {{ISI:000172155800006}},
DA = {{2020-08-06}},
}

@article{ ISI:000173317500003,
Author = {Lee, CF and Lin, SJ and Lewis, C},
Title = {{Devising an integrated methodology for analyzing energy used and CO2
   emissions from Taiwan's petrochemical industries}},
Journal = {{JOURNAL OF ENVIRONMENTAL MANAGEMENT}},
Year = {{2001}},
Volume = {{63}},
Number = {{4}},
Pages = {{377-385}},
Month = {{DEC}},
Abstract = {{Input-output modeling and multiplier analysis are used to assess
   Taiwan's five petrochemical industries, based upon their economic
   contribution and potential impacts on energy consumption and CO2
   emission. In addition, a consolidated index system was developed for
   evaluating energy and economic efficiencies as well as targets for CO2
   reduction. Results indicate that petrochemical materials (PM) make a
   major contribution to economic development, with lesser contributions
   from plastic materials (PL) and artificial fibres (AF). PM has the
   highest energy multiplier while PL has the largest induced potential for
   energy consumption. Plastic and rubber products (PP, RP) are relatively
   insignificant energy consumers. AF has the highest CO2 multiplier, and
   its induced potential for CO2 emission is the most significant. The
   consolidated index shows that the upstream petrochemical industries
   perform rather poorly in an integrated view of economic, energy, and CO2
   emission, and should be seen as the primary targets for CO2 reduction.
   Investment of the petrochemical industries in Taiwan should be adjusted
   to improve energy efficiency, economic bases, and lower CO2 emissions.
   (C) 2001 Academic Press.}},
Publisher = {{ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD}},
Address = {{24-28 OVAL RD, LONDON NW1 7DX, ENGLAND}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Lin, SJ (Corresponding Author), Natl Cheng Kung Univ, Dept Environm Engn, Tainan 70101, Taiwan.
   Natl Cheng Kung Univ, Dept Environm Engn, Tainan 70101, Taiwan.
   Natl Cheng Kung Univ, Dept Resources Engn, Tainan 70101, Taiwan.}},
DOI = {{10.1006/jema.2001.0479}},
ISSN = {{0301-4797}},
EISSN = {{1095-8630}},
Keywords = {{petrochemical industries; input-output analysis; inter-industry linkage;
   energy multiplier; CO2 multiplier; consolidated index}},
Keywords-Plus = {{INPUT-OUTPUT-ANALYSIS; CONSUMPTION}},
Research-Areas = {{Environmental Sciences \& Ecology}},
Web-of-Science-Categories  = {{Environmental Sciences}},
Author-Email = {{t15197@mail.ncku.edu.tw}},
Cited-References = {{{*}ACC OFF EX YUAN, 1999, TAIW INT INP OUTP LI.
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Number-of-Cited-References = {{27}},
Times-Cited = {{4}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{16}},
Journal-ISO = {{J. Environ. Manage.}},
Doc-Delivery-Number = {{512GW}},
Unique-ID = {{ISI:000173317500003}},
DA = {{2020-08-06}},
}

@article{ ISI:000176111200006,
Author = {Kusunoki, S and Sugi, M and Kitoh, A and Kobayashi, C and Takano, K},
Title = {{Atmospheric seasonal predictability experiments by the JMA AGCM}},
Journal = {{JOURNAL OF THE METEOROLOGICAL SOCIETY OF JAPAN}},
Year = {{2001}},
Volume = {{79}},
Number = {{6}},
Pages = {{1183-1206}},
Month = {{DEC}},
Abstract = {{Atmospheric seasonal predictability is investigated using the Japan
   Meteorological Agency (JMA) Atmospheric General Circulation Model (AGCM)
   which is a global spectral model of T63 resolution used for former
   operational one-month forecasts. Four-month ensemble integrations were
   performed from nine consecutive days of initial condition preceding the
   target season. All four seasons in the 15-year period from 1979 to 1993
   are chosen as the target seasons. The model was forced with observed sea
   surface temperature (SST) during the time integrations.
   Verification by the anomaly correlation of seasonal averaged 500 hPa
   height are summarized as follows. (1) In terms of a 15-year mean,
   ensemble average forecasts tend to have higher skill than means of
   individual forecasts, persistence forecasts and climatological forecasts
   over the whole globe. (2) In the Northern Hemisphere, skill is high in
   spring and winter, and low in summer and autumn. (3) Skill is higher
   over East Asia and North America, than over Europe and Atlantic regions.
   In winter, the relatively higher skill over East Asia and North America
   can be attributed to reasonable reproducibility of Western Pacific (WP)
   and Pacific/North American (PNA) teleconnection patterns by the model.
   (4) A larger ensemble size improves the skill of the model both for
   extratropical regions and the tropics, and for all four seasons. (5) The
   skill of one-month lead time forecasts is lower than that of no lead
   time forecasts for all regions and all seasons. Focusing on the Northern
   Hemisphere, the relatively large skill degradation with respect to lead
   time is striking in spring, which suggests that the model is more
   sensitive to initial conditions in spring than in summer and autumn. (6)
   Skill enhancement for strong El Nino and the Southern Oscillation (ENSO)
   years is generally evident over the whole globe, but is not so striking
   in the Northern Hemisphere. Skill over North America increases for ENSO
   years, but there is no clear skill enhancement over the Europe and
   Atlantic regions.
   The model's ability to reproduce the interannual variability of
   precipitation was also investigated. Geographycal distributions of
   interannual temporal correlation coefficients between observed
   precipitation, and model ensemble average forecast precipitation show
   that correlations are generally higher in the tropics than in the
   extratropics for all seasons. In the tropics, skill is relatively higher
   in the equatorial eastern Pacific ocean and lower over India. The model
   has difficulty in simulating the interannual variability of
   precipitation for the Indian summer monsoon season and for the East
   Asian rainy season in summer, which may originate from the model's poor
   climatology over these regions in summer.}},
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 = {{Kusunoki, S (Corresponding Author), Japan Meteorol Agcy, Climate Predict Div, Climate \& Marine Dept, Chiyoda Ku, 1-3-4 Ote Machi, Tokyo 1008122, Japan.
   Japan Meteorol Agcy, Climate Predict Div, Climate \& Marine Dept, Chiyoda Ku, Tokyo 1008122, Japan.
   Japan Meteorol Agcy, Climate Res Dept, Meteorol Res Inst, Tokyo 1008122, Japan.}},
DOI = {{10.2151/jmsj.79.1183}},
ISSN = {{0026-1165}},
EISSN = {{2186-9057}},
Keywords-Plus = {{GENERAL-CIRCULATION MODELS; SEA-SURFACE TEMPERATURE; SIMPLE BIOSPHERE
   MODEL; EL-NINO; ENSEMBLE SIZE; GLOBAL-MODEL; VARIABILITY; FORECASTS;
   MONSOON; SIMULATIONS}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{s-kusunoki@met.kishou.go.jp}},
ResearcherID-Numbers = {{Kitoh, Akio/F-1765-2010
   sugi, masato/P-9076-2014}},
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