text:
V9, P303, DOI 10.1007/BF00204745.
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Number-of-Cited-References = {{36}},
Times-Cited = {{42}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{4}},
Journal-ISO = {{Geology}},
Doc-Delivery-Number = {{569NB}},
Unique-ID = {{ISI:000176607500014}},
DA = {{2020-08-06}},
}

@article{ ISI:000176325500011,
Author = {Mariotti, A and Struglia, MV and Zeng, N and Lau, KM},
Title = {{The hydrological cycle in the Mediterranean region and implications for
   the water budget of the Mediterranean Sea}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2002}},
Volume = {{15}},
Number = {{13}},
Pages = {{1674-1690}},
Month = {{JUL}},
Abstract = {{The hydrological cycle in the Mediterranean region is analyzed focusing
   on climatology and interannual to interdecadal variability, in
   particular long-term changes related to the well-established North
   Atlantic Oscillation (NAO) teleconnection. Recent atmospheric reanalyses
   and observational datasets are used: precipitation, evaporation, and
   moisture flux from 50 yr of NCEP's and 15 yr of ECMWF's reanalyses;
   precipitation from the Climate Prediction Center Merged Analysis of
   Precipitation (CMAP) and the East Anglia University Climate Research
   Unit (CRU) datasets; and evaporation from the University of
   Wisconsin-Milwaukee (UWM) Comprehensive Ocean-Atmosphere Data Set
   (COADS). A budget analysis is performed to study contributions to the
   freshwater flux into the Mediterranean Sea, including atmospheric as
   well as river discharge inputs. The total river discharge is derived
   using historical time series from Mediterranean Hydrological Cycle
   Observing System (MED-HYCOS) and Global Runoff Data Center (GRDC)
   archives.
   Mediterranean-averaged precipitation during the period 1979-93 has an
   annual mean ranging among datasets from 331 to 477 mm yr 21, with a
   seasonal cycle amplitude of similar to700 mm yr(-1). Evaporation is
   estimated in the range of 934-1176 mm yr(-1) with a seasonal cycle
   amplitude of similar to1000 mm yr(-1). The excess of evaporation over
   precipitation gives an annual mean Mediterranean Sea water loss ranging
   among datasets approximately from 500 to 700 mm yr(-1). The annual mean
   river discharge is 100 mm yr(-1), somewhat smaller than previous
   estimates using similar approaches. Water loss to the atmosphere and
   riverine inputs combined lead to an estimated Mediterranean freshwater
   deficit of about 500 mm yr(-1), consistent with most oceanographically
   based estimates of the water flux from the Atlantic Ocean at the
   Gibraltar Strait.
   On interannual to interdecadal timescales, during the period 1948-98,
   the Mediterranean atmospheric winter water deficit is positively
   correlated with the NAO and has been increasing due to the long-term
   positive anomalies of the NAO since the early 1970s. Precipitation,
   which is also significantly correlated with the NAO, appears to be
   mostly responsible for this since no significant correlation is found
   for evaporation. Over the 50-yr period the Mediterranean atmospheric
   water deficit increased by about 24\% in the winter season, and by 9\%
   annually. Given the pattern of the NAO-related precipitation anomalies,
   this change is likely to have occurred primarily north of 35degreesN.
   The results presented here suggest that in response to the changes in
   the freshwater flux significant variations in the characteristics of
   Mediterranean waters and the Gibraltar flux may also have occurred
   during this period, mostly driven by the influence of the NAO.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Mariotti, A (Corresponding Author), Univ Maryland, Earth Syst Sci Interdisciplinary Ctr, 2207 Comp \& Space Sci Bldg, College Pk, MD 20742 USA.
   Univ Maryland, Earth Syst Sci Interdisciplinary Ctr, College Pk, MD 20742 USA.
   Univ Maryland, Dept Meteorol, College Pk, MD 20742 USA.
   ENEA, Climate Sect, Rome, Italy.
   NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA.}},
DOI = {{10.1175/1520-0442(2002)015<1674:THCITM>2.0.CO;2}},
ISSN = {{0894-8755}},
EISSN = {{1520-0442}},
Keywords-Plus = {{NORTH-ATLANTIC OSCILLATION; GLOBAL PRECIPITATION; ATMOSPHERIC MOISTURE;
   REANALYSIS PROJECT; GAUGE OBSERVATIONS; PART II; CLIMATE; MODEL;
   VARIABILITY; NCEP/NCAR}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{annarita.mariotti@casaccia.enea.it}},
ResearcherID-Numbers = {{Zeng, Ning/A-3130-2008
   Lau, William K/E-1510-2012
   }},
ORCID-Numbers = {{Zeng, Ning/0000-0002-7489-7629
   Lau, William K/0000-0002-3587-3691
   Struglia, Maria Vittoria/0000-0002-0821-333X}},
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Number-of-Cited-References = {{43}},
Times-Cited = {{246}},
Usage-Count-Last-180-days = {{3}},
Usage-Count-Since-2013 = {{28}},
Journal-ISO = {{J. Clim.}},
Doc-Delivery-Number = {{564QR}},
Unique-ID = {{ISI:000176325500011}},
DA = {{2020-08-06}},
}

@article{ ISI:000176325500016,
Author = {Hawkins, TW and Ellis, AW and Skindlov, JA and Reigle, D},
Title = {{Intra-annual analysis of the North American snow cover-monsoon
   teleconnection: Seasonal forecasting utility}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2002}},
Volume = {{15}},
Number = {{13}},
Pages = {{1743-1753}},
Month = {{JUL}},
Abstract = {{Areal extents of monthly and seasonal North American snow cover were
   correlated with precipitation totals, precipitation frequency, and
   severe weather associated with the North American monsoon. Significant
   relationships were found to exist between monsoon variables and
   snow-cover extent over western North America.
   Synoptic composites of the summertime atmosphere revealed that during
   years of low snow-cover extent, 500-mb heights were higher across much
   of the United States and 850-mb specific humidity values were increased
   over the desert southwest compared with high snow-cover extent years.
   Seemingly, displacement of the 500-mb ridge across the United States
   displaces the Four Corners high, which in turn affects the strength of
   low-level moisture advection into the southwestern United States.
   In beginning to assess the possibility of anticipating the strength of
   the North American monsoon using winter and spring snow-cover extent,
   data for anomalously large and small snow-cover years (50\% of the data
   record) were input into stepwise multiple regressions. Using the limited
   data record, results showed that winter and spring snow-cover variables
   explained significant portions of the variance in precipitation totals
   (83\%), precipitation frequency (95\%), hail (81\%), wind (82\%), and
   total severe weather (98\%) for the monsoon region. The results lead to
   optimism regarding the development of seasonal forecasting algorithms
   that are centered upon the use of winter and spring snow-cover extent to
   assess the potential intensity of the subsequent North American monsoon
   season. Accurate prediction of general monsoon intensity several months
   in advance would be invaluable to many different aspects of life in
   southwestern North America.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Hawkins, TW (Corresponding Author), Arizona State Univ, Dept Geog, Box 870104, Tempe, AZ 85287 USA.
   Arizona State Univ, Dept Geog, Tempe, AZ 85287 USA.
   Salt River Project, Water Resource Operat, Phoenix, AZ USA.}},
DOI = {{10.1175/1520-0442(2002)015<1743:IAAOTN>2.0.CO;2}},
ISSN = {{0894-8755}},
Keywords-Plus = {{SOUTHWEST UNITED-STATES; SUMMER RAINFALL; INDIAN MONSOON; PRECIPITATION;
   TEMPERATURE; VARIABILITY; HEMISPHERE; MAXIMUM}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
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Number-of-Cited-References = {{26}},
Times-Cited = {{25}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{3}},
Journal-ISO = {{J. Clim.}},
Doc-Delivery-Number = {{564QR}},
Unique-ID = {{ISI:000176325500016}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000184726500002,
Author = {Yan, YY},
Title = {{Temporal and spatial patterns of seasonal precipitation variability in
   China, 1951-1999}},
Journal = {{PHYSICAL GEOGRAPHY}},
Year = {{2002}},
Volume = {{23}},
Number = {{4}},
Pages = {{281-301}},
Month = {{JUL-AUG}},
Abstract = {{Rainfall variability in China for the period from 1951 to 1999 was
   investigated. Monthly rainfall data for 160 stations were obtained from
   the Chinese Academy of Meteorological Sciences. Mean seasonal rainfall
   amounts were grouped into four distinct precipitation regions by cluster
   analysis. These regions differed in size and extent in each season and
   were related to the rainfall-generating mechanism operating at that time
   of year. The Asian monsoon played a major role in shaping the
   precipitation regime. Local topography also helped in casting the
   seasonal variability patterns within regions. To understand the impact
   of large scale circulation on rainfall variability, areally averaged
   anomaly percentages were correlated with major atmospheric
   teleconnection features. It was discovered that the Polar-Eurasia (POL)
   and Arctic Oscillation (AO) index were positively associated with winter
   precipitation, indicating the significance of the winter monsoon in
   producing the rainfall pattern. Negligible effects of the Southern
   Oscillation Index (SOI), West Pacific (WP), and North Pacific (NP)
   patterns on precipitation were observed.}},
Publisher = {{V H WINSTON \& SON INC}},
Address = {{360 SOUTH OCEAN BLVD, PH-B, PALM BEACH, FL 33480 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Yan, YY (Corresponding Author), Hong Kong Baptist Univ, Dept Geog, Kowloon, Hong Kong, Peoples R China.
   Hong Kong Baptist Univ, Dept Geog, Kowloon, Hong Kong, Peoples R China.}},
DOI = {{10.2747/0272-3646.23.4.281}},
ISSN = {{0272-3646}},
Keywords = {{precipitation variability; monsoon; teleconnections}},
Keywords-Plus = {{NORTHERN-HEMISPHERE WINTER; GEOPOTENTIAL HEIGHT; SUMMER RAINFALL;
   ARCTIC-OSCILLATION; MONSOON RAINFALL; TELECONNECTIONS; CIRCULATION;
   PACIFIC; ENSO; ASSOCIATIONS}},
Research-Areas = {{Environmental Sciences \& Ecology; Physical Geography; Geology;
   Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Environmental Sciences; Geography, Physical; Geosciences,
   Multidisciplinary; Meteorology \& Atmospheric Sciences}},
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Times-Cited = {{5}},
Usage-Count-Last-180-days = {{2}},
Usage-Count-Since-2013 = {{7}},
Journal-ISO = {{Phys. Geogr.}},
Doc-Delivery-Number = {{711EK}},
Unique-ID = {{ISI:000184726500002}},
DA = {{2020-08-06}},
}

@article{ ISI:000176656400001,
Author = {Liu, JP and Martinson, DG and Yuan, XJ and Rind, D},
Title = {{Evaluating Antarctic sea ice variability and its teleconnections in
   global climate models}},
Journal = {{INTERNATIONAL JOURNAL OF CLIMATOLOGY}},
Year = {{2002}},
Volume = {{22}},
Number = {{8}},
Pages = {{885-900}},
Month = {{JUN 30}},
Abstract = {{This study evaluates simulated Antarctic sea ice edge (SIE) variability
   and its teleconnections in three global coupled climate models (GISS,
   NCAR and GFDL) against the observations. All models do a reasonable job
   in simulating the seasonal advance and retreat of the Antarctic sea ice
   fields. The simulated GISS and NCAR SIE distributions are in agreement
   with observations in summer and autumn, whereas the GFDL model does best
   in spring and winter. A common problem is the poor simulation of the
   observed SIE in the Weddell Sea. All models are not particularly good at
   simulating the observed regionally varying SIE trends. A comparison of
   dominant empirical orthogonal function modes of surface air temperature
   (SAT) variability in each model associated with observed modes show that
   the models generally capture features of the more prominent covarying
   spatial patterns such as an El Nino-southern oscillation (ENSO)-like
   pattern in the tropical Pacific.
   The simulated teleconnection patterns between detrended Antarctic SIE
   anomalies and detrended global SAT anomalies in each model are evaluated
   for comparison with observed teleconnection patterns. All models capture
   the ENSO-like phenomenon to some degree. Also, the GISS and NCAR models
   capture the Antarctic dipole pattern and meridional banding structure
   through the Pacific. The Antarctic SIE regions showing the strongest
   extrapolar teleconnections differ among the models and between the
   models and observations. Almost all models miss the observed
   polar-extrapolar teleconnections in the central Indian, western extreme
   of the tropical and southern Pacific, and over the tropical continents.
   Copyright (C) 2002 Royal Meteorological Society.}},
Publisher = {{JOHN WILEY \& SONS LTD}},
Address = {{BAFFINS LANE CHICHESTER, W SUSSEX PO19 1UD, ENGLAND}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Liu, JP (Corresponding Author), NASA, Goddard Space Flight Ctr, Inst Space Studies, 2880 Broadway, New York, NY 10025 USA.
   NASA, Goddard Space Flight Ctr, Inst Space Studies, New York, NY 10025 USA.
   Columbia Univ, Dept Earth \& Environm Sci, Palisades, NY 10964 USA.
   Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY 10964 USA.}},
DOI = {{10.1002/joc.770}},
ISSN = {{0899-8418}},
Keywords = {{Antarctic sea ice edge; global climate models; teleconnection patterns;
   ENSO bellingshausen; Amundsen, Ross and Weddell Seas}},
Keywords-Plus = {{SOUTHERN OSCILLATION; SYSTEM-MODEL; OCEAN; TEMPERATURE; EXTENT;
   SENSITIVITY; ASYMMETRY; LAYER}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
ResearcherID-Numbers = {{Yuan, Xiaojun/AAI-7770-2020
   LIU, JIPING/N-6696-2016
   }},
ORCID-Numbers = {{Yuan, Xiaojun/0000-0002-6530-1619}},
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Number-of-Cited-References = {{41}},
Times-Cited = {{15}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{4}},
Journal-ISO = {{Int. J. Climatol.}},
Doc-Delivery-Number = {{570KA}},
Unique-ID = {{ISI:000176656400001}},
DA = {{2020-08-06}},
}

@article{ ISI:000178964100002,
Author = {Mariotti, A and Zeng, N and Lau, KM},
Title = {{Euro-Mediterranean rainfall and ENSO - a seasonally varying relationship}},
Journal = {{GEOPHYSICAL RESEARCH LETTERS}},
Year = {{2002}},
Volume = {{29}},
Number = {{12}},
Month = {{JUN 15}},
Abstract = {{{[}1] Using observational datasets and atmospheric reanalyses, we show
   that interannual variability of rainfall in the Euro-Mediterranean
   sector is significantly influenced by ENSO in a way that is seasonally
   varying. Spatially coherent correlation patterns are found in central
   and eastern Europe during winter and spring, and in western Europe and
   the Mediterranean region during autumn and spring. A composite analysis
   of ENSO events indicates that during an El Nino western Mediterranean
   rainfall has a 10\% increase (decrease) in the autumn preceeding (spring
   after) the mature phase of an event, corresponding to a rainy season
   arriving (retreating) earlier compared to the climatology. The
   atmospheric reanalyses show that an anomalous atmospheric circulation
   and moisture transport extending from the Atlantic Ocean into the
   Euro-Mediterranean region accompanies the observed rainfall anomalies.
   Multidecadal variations characterize the ENSO Euro-Mediterranean
   relationship during the 20th century.}},
Publisher = {{AMER GEOPHYSICAL UNION}},
Address = {{2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Mariotti, A (Corresponding Author), ENEA, Natl Agcy, Climate Sect, Via Anguillarese 301-SP 91,SM Galeria, I-00060 Rome, Italy.
   ENEA, Natl Agcy, Climate Sect, I-00060 Rome, Italy.
   Univ Maryland, Dept Meteorol, College Pk, MD 20742 USA.
   Univ Maryland, Ctr Earth Syst Sci, College Pk, MD 20742 USA.
   NASA, Goddard Space Flight Ctr, Climate \& Radiat Branch, Greenbelt, MD 20771 USA.}},
DOI = {{10.1029/2001GL014248}},
Article-Number = {{1621}},
ISSN = {{0094-8276}},
Keywords-Plus = {{NORTH-ATLANTIC OSCILLATION; NINO SOUTHERN OSCILLATION; EL-NINO; CLIMATE
   VARIABILITY; PRECIPITATION; TELECONNECTION; TEMPERATURES; PATTERNS}},
Research-Areas = {{Geology}},
Web-of-Science-Categories  = {{Geosciences, Multidisciplinary}},
ResearcherID-Numbers = {{Zeng, Ning/A-3130-2008}},
ORCID-Numbers = {{Zeng, Ning/0000-0002-7489-7629}},
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Number-of-Cited-References = {{23}},
Times-Cited = {{139}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{16}},
Journal-ISO = {{Geophys. Res. Lett.}},
Doc-Delivery-Number = {{610MP}},
Unique-ID = {{ISI:000178964100002}},
DA = {{2020-08-06}},
}

@article{ ISI:000176248400011,
Author = {Chiew, FHS and McMahon, TA},
Title = {{Global ENSO-streamflow teleconnection, streamflow forecasting and
   interannual variability}},
Journal = {{HYDROLOGICAL SCIENCES JOURNAL-JOURNAL DES SCIENCES HYDROLOGIQUES}},
Year = {{2002}},
Volume = {{47}},
Number = {{3}},
Pages = {{505-522}},
Month = {{JUN}},
Abstract = {{El Ni (n) over tildeo Southern Oscillation (ENSO) has been linked to
   climate anomalies throughout the world. This paper presents an overview
   of global ENSO-streamflow teleconnection and identifies regions where
   the relationship may be exploited to forecast streamflow several months
   ahead. The teleconnection is investigated by fitting a first harmonic to
   24-month El Ni (n) over tildeo streamflow composites from 581 catchments
   worldwide and the potential for forecasting is investigated by
   calculating the tag correlation between streamflow and two indicators of
   ENSO. The analyses indicate clear ENSO-streamflow teleconnections in
   many catchments, some of which are consistent across large geographical
   regions. Strong and regionally consistent ENSO-streamflow
   teleconnections are identified in Australia and New Zealand, South and
   Central America, and weaker signals are identified in some parts of
   Africa and North America. The results suggest that the ENSO-streamflow
   relationship and the serial correlation in streamflow can be used to
   successfully forecast streamflow. The streamflow forecasts can be used
   to help manage water resources, particularly in systems with high
   interannual variability in Australia, southern and drier parts of Africa
   and some areas of North America.}},
Publisher = {{IAHS PRESS, INST HYDROLOGY}},
Address = {{C/O FRANCES WATKINS, WALLINGFORD OX10 8BB, ENGLAND}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Chiew, FHS (Corresponding Author), Univ Melbourne, Cooperat Res Ctr Catchment Hydrol, Dept Civil \& Environm Engn, Melbourne, Vic 3010, Australia.
   Univ Melbourne, Cooperat Res Ctr Catchment Hydrol, Dept Civil \& Environm Engn, Melbourne, Vic 3010, Australia.}},
DOI = {{10.1080/02626660209492950}},
ISSN = {{0262-6667}},
Keywords = {{streamflow; El Nino; southern oscillation; teleconnection; forecasting;
   global; harmonic analysis}},
Keywords-Plus = {{NINO SOUTHERN OSCILLATION; EL-NINO; UNITED-STATES; RAINFALL; PATTERNS;
   PRECIPITATION; TEMPERATURE; DROUGHT}},
Research-Areas = {{Water Resources}},
Web-of-Science-Categories  = {{Water Resources}},
ResearcherID-Numbers = {{McMahon, Thomas/AAD-9845-2020
   Chiew, Francis/A-9743-2011}},
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Number-of-Cited-References = {{23}},
Times-Cited = {{119}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{34}},
Journal-ISO = {{Hydrol. Sci. J.-J. Sci. Hydrol.}},
Doc-Delivery-Number = {{563GR}},
Unique-ID = {{ISI:000176248400011}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000175349600005,
Author = {Rodriguez-Fonseca, B and Serrano, E},
Title = {{Winter 10-day coupled patterns between geopotential height and Iberian
   Peninsula rainfall using the ECMWF precipitation reanalysis}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2002}},
Volume = {{15}},
Number = {{11}},
Pages = {{1309-1321}},
Month = {{JUN 1}},
Abstract = {{Ten-day winter anomalous precipitation variability in the Iberian
   Peninsula (IP), related to the North Atlantic atmospheric general
   circulation, is analyzed using 24-h forecast ECMWF precipitation data
   over 1979-96. The three main modes that explain the 10-day winter
   precipitation variability are described using the empirical orthogonal
   function (EOF) analysis. Singular value decomposition (SVD) analysis
   between the anomalous geo-potential height for different levels and the
   IP precipitation is used as a tool to establish the relation between the
   precipitation and the North Atlantic atmospheric general circulation,
   showing how the first three SVD modes collect practically all possible
   precipitation-atmosphere links in these timescales. These resultant SVD
   atmospheric patterns are related to other known teleconnection patterns,
   such as the Arctic Oscillation (AO), the North Atlantic Oscillation
   (NAO), the Scandinavian pattern (SCA), and the east Atlantic pattern
   (EA). At the same time, the main results are compared with those
   obtained from station precipitation data. The good agreement with the
   significant coupled patterns obtained when using observed precipitation
   data is shown as a further way of validating the precipitation 24-h
   forecast of the ECMWF dataset for these types of studies.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Rodriguez-Fonseca, B (Corresponding Author), Univ Complutense Madrid, Fac CC Fis, Dept Geofis \& Meteorol, Cuidad Univ S-N, E-28040 Madrid, Spain.
   Univ Complutense Madrid, Fac CC Fis, Dept Geofis \& Meteorol, E-28040 Madrid, Spain.}},
DOI = {{10.1175/1520-0442(2002)015<1309:WDCPBG>2.0.CO;2}},
ISSN = {{0894-8755}},
EISSN = {{1520-0442}},
Keywords-Plus = {{NORTH-ATLANTIC OSCILLATION; SEA-SURFACE-TEMPERATURE; SINGULAR-VALUE
   DECOMPOSITION; ATMOSPHERIC CIRCULATION; TEMPORAL PATTERNS; VARIABILITY;
   TELECONNECTIONS; TRENDS; EUROPE; MODES}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{brfonsec@fis.ucm.es}},
ResearcherID-Numbers = {{Serrano, Encarna/F-6346-2016
   Rodriguez-Fonseca, Belen/I-8276-2017}},
ORCID-Numbers = {{Serrano, Encarna/0000-0003-0031-0562
   Rodriguez-Fonseca, Belen/0000-0002-5261-7083}},
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Number-of-Cited-References = {{32}},
Times-Cited = {{12}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{3}},
Journal-ISO = {{J. Clim.}},
Doc-Delivery-Number = {{547UC}},
Unique-ID = {{ISI:000175349600005}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000178888300139,
Author = {Kirtman, BP and Shukla, J},
Title = {{Interactive coupled ensemble: A new coupling strategy for CGCMs}},
Journal = {{GEOPHYSICAL RESEARCH LETTERS}},
Year = {{2002}},
Volume = {{29}},
Number = {{10}},
Month = {{MAY 15}},
Abstract = {{{[}1] This paper presents a new strategy for coupling state-of-the-art
   oceanic and atmospheric general circulation models. The procedure is to
   use multiple realizations of the atmospheric GCM coupled to a single
   realization of the ocean GCM. The ensemble mean state of the atmospheric
   GCM fluxes are coupled to the ocean model thereby affecting the
   evolution of the coupled system. The traditional approach for generating
   a coupled ensemble is to apply the ensemble averaging to a collection of
   individual realizations a posteriori. This interactive ensemble
   technique is distinct from the traditional procedure because here the
   ensemble mean of the atmospheric models continuously interacts with the
   ocean model as the coupled system evolves. Simulation experiments with
   and without the interactive ensemble are described. The interactive
   ensemble coupled model produces realistic ENSO events that are
   irregular. This technique also dramatically improves the simulation of
   the global teleconnection associated with ENSO, and the ENSO-monsoon
   relationship.}},
Publisher = {{AMER GEOPHYSICAL UNION}},
Address = {{2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Kirtman, BP (Corresponding Author), Ctr Ocean Land Atmosphere Studies, 4041 Powder Mill Rd,Suite 302, Calverton, MD 20705 USA.
   Ctr Ocean Land Atmosphere Studies, Calverton, MD 20705 USA.}},
DOI = {{10.1029/2002GL014834}},
Article-Number = {{1367}},
ISSN = {{0094-8276}},
Keywords-Plus = {{SOUTHERN OSCILLATION; ENSO PREDICTABILITY; SEASONAL CYCLE; MODEL;
   VARIABILITY; PREDICTION; MONSOON; CLIMATE; CHAOS}},
Research-Areas = {{Geology}},
Web-of-Science-Categories  = {{Geosciences, Multidisciplinary}},
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Number-of-Cited-References = {{15}},
Times-Cited = {{97}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{4}},
Journal-ISO = {{Geophys. Res. Lett.}},
Doc-Delivery-Number = {{609DL}},
Unique-ID = {{ISI:000178888300139}},
DA = {{2020-08-06}},
}

@article{ ISI:000178888300102,
Author = {Liu, Z and Wu, L and Gallimore, R and Jacob, R},
Title = {{Search for the origins of Pacific decadal climate variability}},
Journal = {{GEOPHYSICAL RESEARCH LETTERS}},
Year = {{2002}},
Volume = {{29}},
Number = {{10}},
Month = {{MAY 15}},
Abstract = {{{[}1] The origin of Pacific decadal climate variability is investigated
   in a coupled ocean-atmosphere general circulation model. The impact of
   regional ocean-atmosphere coupling and oceanic teleconnection on decadal
   variability is evaluated by performing a set of specifically designed
   experiments. It is found that decadal variability in the tropical and
   North Pacific originates predominantly from local coupled
   ocean-atmosphere processes within the tropical and North Pacific region,
   respecively. Furthermore, tropical Pacific decadal variability appears
   to be associated with higher baroclinic modes and can be enhanced
   substantially by extratropical-tropical oceanic teleconnection.}},
Publisher = {{AMER GEOPHYSICAL UNION}},
Address = {{2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Liu, Z (Corresponding Author), Univ Wisconsin, Ctr Climate Res, 1225 W Dayton St, Madison, WI 53706 USA.
   Univ Wisconsin, Ctr Climate Res, Madison, WI 53706 USA.
   Argonne Natl Lab, Argonne, IL 60439 USA.}},
DOI = {{10.1029/2001GL013735}},
Article-Number = {{1404}},
ISSN = {{0094-8276}},
EISSN = {{1944-8007}},
Keywords = {{tropical decadal mode; North Pacific decadal mode;
   extratropical/tropical interaction}},
Keywords-Plus = {{NORTH PACIFIC; ENSO; OSCILLATION; AMERICA}},
Research-Areas = {{Geology}},
Web-of-Science-Categories  = {{Geosciences, Multidisciplinary}},
Author-Email = {{zliu3@facstaff.wisc.edu}},
ResearcherID-Numbers = {{Jacob, Robert/D-2580-2011}},
ORCID-Numbers = {{Jacob, Robert/0000-0002-9444-6593}},
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Number-of-Cited-References = {{16}},
Times-Cited = {{55}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{9}},
Journal-ISO = {{Geophys. Res. Lett.}},
Doc-Delivery-Number = {{609DL}},
Unique-ID = {{ISI:000178888300102}},
DA = {{2020-08-06}},
}

@article{ ISI:000175248900007,
Author = {Kinter, JL and Miyakoda, K and Yang, S},
Title = {{Recent change in the connection from the Asian monsoon to ENSO}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2002}},
Volume = {{15}},
Number = {{10}},
Pages = {{1203-1215}},
Month = {{MAY 15}},
Abstract = {{The Asian monsoon and El Nino-Southern Oscillation (ENSO) are known to
   interact with each other. In this paper, four primary indices (the
   Indian monsoon rainfall index, the Webster and Yang monsoon index, the
   tropical-wide oscillation index, and the Southern Oscillation index)
   that characterize the temporal variation of these complex, chaotic and
   quasi-oscillatory phenomena are used to assess the action from the Asian
   monsoon to ENSO, that is, the linkage between the strong/weak monsoon
   and La Nina/El Nino. The evolution of the four previously documented
   indices and other auxiliary data over a 43-yr period is examined using
   the observed database and the reanalysis of the National Centers for
   Environmental Prediction. The Asian monsoon and ENSO intersect in a
   common area, namely, the warm pool in the western tropical Pacific. This
   region (e. g., 10degreesS-5degreesN, 110degrees-170degreesE) is located
   at the longitudinally central portion of the Walker circulation and also
   the equatorial end of the Indo-Pacific meridional overturning cell that
   is part of the zonal mean Hadley circulation. In recent decades, the
   connection between the monsoon and ENSO has changed considerably. This
   change is related to the atmospheric circulation over the entire North
   Pacific Ocean, which entered a new regime in about 1976. Before 1976,
   the correlations among the four primary indices, and those between the
   indices and the Nino-3 index of sea surface temperature, were strong. In
   recent decades, the ocean temperature in the entire North Pacific became
   considerably colder. The lower-tropospheric winds became simultaneously
   more cyclonic over the North Pacific. ENSO is now related to atmospheric
   fluctuations both in the Indian sector and in northeastern China. The
   western North Pacific monsoon in the vicinity of the Philippine Islands
   (9degrees-19degreesN, 139degrees-141degreesE) may play an important role
   together with the off-equatorial ocean heat content in a larger region
   (5degrees-15degreesN, 135degrees-170degreesE) in maintaining or even
   increasing ENSO activities.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Kinter, JL (Corresponding Author), Ctr Ocean Land Atmosphere Studies, Inst Global Environm \& Soc, 4041 Powder Mill Rd,Suite 302, Calverton, MD 20705 USA.
   Ctr Ocean Land Atmosphere Studies, Inst Global Environm \& Soc, Calverton, MD 20705 USA.
   George Mason Univ, Sch Computat Sci, Fairfax, VA 22030 USA.
   Natl Weather Serv, Climate Predict Ctr, Natl Ctr Environm Predict, NOAA, Camp Springs, MD USA.}},
DOI = {{10.1175/1520-0442(2002)015<1203:RCITCF>2.0.CO;2}},
ISSN = {{0894-8755}},
EISSN = {{1520-0442}},
Keywords-Plus = {{SEA-SURFACE TEMPERATURE; TROPICAL-WIDE TELECONNECTION; INTERANNUAL TIME
   SCALES; INDIAN-SUMMER MONSOON; TRADE-WIND SYSTEM; NORTH PACIFIC;
   INTERDECADAL VARIABILITY; SOUTHERN-OSCILLATION; EQUATORIAL PACIFIC;
   RAINFALL}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{kinter@cola.iges.org}},
ResearcherID-Numbers = {{Yang, Song/B-4952-2009}},
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Number-of-Cited-References = {{62}},
Times-Cited = {{126}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{25}},
Journal-ISO = {{J. Clim.}},
Doc-Delivery-Number = {{546AC}},
Unique-ID = {{ISI:000175248900007}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000175283200007,
Author = {Pachauri, S and Spreng, D},
Title = {{Direct and indirect energy requirements of households in India}},
Journal = {{ENERGY POLICY}},
Year = {{2002}},
Volume = {{30}},
Number = {{6}},
Pages = {{511-523}},
Month = {{MAY}},
Abstract = {{This study is based on the 115 sector classification input-output tables
   for India for the years 1983-84, 1989-90 and 1993-94. Calculated total
   primary energy intensities along,with private final consumption
   expenditures are used as a basis for determining the indirect energy
   requirements of Indian households. Results reveal that total household
   energy consumption is about evenly divided between direct and indirect
   energy and together comprises 75\% of the total energy consumption of
   India. Most of household energy consumed directly is still
   non-commercial and the consumption of food is responsible for about half
   the indirect energy consumption. Household energy requirements have
   increased significantly, both in total and per capita terms over this
   time period. The commercial component of direct household energy
   consumption and the indirect energy requirements have increased
   continuously. The main drivers of this increase hake been ( 1) the
   growing expenditures per capita, (2) population and (3) increasing
   energy intensity in the food and agricultural sectors. (C) 2002 Elsevier
   Science Ltd. All rights reserved.}},
Publisher = {{ELSEVIER SCI LTD}},
Address = {{THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Pachauri, S (Corresponding Author), ETH Zentrum WEC, Swiss Fed Inst Technol, Ctr Energy Policy \& Econ, CH-8092 Zurich, Switzerland.
   ETH Zentrum WEC, Swiss Fed Inst Technol, Ctr Energy Policy \& Econ, CH-8092 Zurich, Switzerland.}},
DOI = {{10.1016/S0301-4215(01)00119-7}},
Article-Number = {{PII S0301-4215(01)00119-7}},
ISSN = {{0301-4215}},
Keywords = {{household energy requirements; household expenditures; total primary
   energy intensities}},
Keywords-Plus = {{INPUT-OUTPUT-ANALYSIS; EMISSIONS; SERVICES; GOODS; INTENSITY; COST}},
Research-Areas = {{Business \& Economics; Energy \& Fuels; Environmental Sciences \&
   Ecology}},
Web-of-Science-Categories  = {{Economics; Energy \& Fuels; Environmental Sciences; Environmental
   Studies}},
ResearcherID-Numbers = {{feng, tingting/A-9545-2012
   Pachauri, Shonali/AAR-7383-2020}},
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Number-of-Cited-References = {{42}},
Times-Cited = {{144}},
Usage-Count-Last-180-days = {{2}},
Usage-Count-Since-2013 = {{32}},
Journal-ISO = {{Energy Policy}},
Doc-Delivery-Number = {{546PU}},
Unique-ID = {{ISI:000175283200007}},
DA = {{2020-08-06}},
}

@article{ ISI:000175579300012,
Author = {Ishman, SE and Sperling, MR},
Title = {{Benthic foraminiferal record of Holocene deep-water evolution in the
   Palmer Deep, western Antarctic Peninsula}},
Journal = {{GEOLOGY}},
Year = {{2002}},
Volume = {{30}},
Number = {{5}},
Pages = {{435-438}},
Month = {{MAY}},
Abstract = {{Benthic foraminiferal data from Ocean Drilling Program Site 1098
   indicate significant changes in deep-water conditions of the Palmer
   Deep, western Antarctic Peninsula margin, throughout the Holocene (13 ka
   to present). The earliest Holocene represents a period of transition
   from the Last Glacial Maximum (LGM). Cold bottom waters, similar to
   saline shelf water (SSW), dominated the middle Holocene. The late
   Holocene in the Palmer Deep has been characterized by alternating
   dominance of circumpolar deep water (CDW) and saline shelf water. These
   changes have global oceanographic and climatic implications. We suggest
   that the middle Holocene bottom-water record, in the absence of
   circumpolar deep water on the western Antarctic Peninsula shelf,
   indicates high saline shelf water production and/or weakened circumpolar
   deep water production during the middle Holocene climatic optimum. The
   late Holocene benthic foraminiferal record indicates rapidly fluctuating
   sea-ice conditions and may indicate a teleconnection between the South
   Pacific and Southern Ocean, thus having implications related to the
   Southern Oscillation Index.}},
Publisher = {{GEOLOGICAL SOC AMERICA, INC}},
Address = {{PO BOX 9140, BOULDER, CO 80301-9140 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Ishman, SE (Corresponding Author), So Illinois Univ, Dept Geol, Carbondale, IL 62901 USA.
   So Illinois Univ, Dept Geol, Carbondale, IL 62901 USA.
   Inst Museum Geol \& Paleontol, Tubingen, Germany.}},
DOI = {{10.1130/0091-7613(2002)030<0435:BFROHD>2.0.CO;2}},
ISSN = {{0091-7613}},
Keywords = {{Antarctica; benthic; bottom water; foraminifera; Holocene}},
Keywords-Plus = {{CONTINENTAL-SHELF; GLACIAL HISTORY; SOUTHERN-OCEAN; ATLANTIC-OCEAN;
   CLIMATE-CHANGE; ICE; SEA; REGION; CIRCULATION; ECOLOGY}},
Research-Areas = {{Geology}},
Web-of-Science-Categories  = {{Geology}},
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