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Number-of-Cited-References = {{77}},
Times-Cited = {{243}},
Usage-Count-Last-180-days = {{4}},
Usage-Count-Since-2013 = {{132}},
Journal-ISO = {{Ecol. Econ.}},
Doc-Delivery-Number = {{435FR}},
Unique-ID = {{ISI:000168867200006}},
DA = {{2020-08-06}},
}

@article{ ISI:000168066100026,
Author = {Okumura, Y and Xie, SP and Numaguti, A and Tanimoto, Y},
Title = {{Tropical Atlantic air-sea interaction and its influence on the NAO}},
Journal = {{GEOPHYSICAL RESEARCH LETTERS}},
Year = {{2001}},
Volume = {{28}},
Number = {{8}},
Pages = {{1507-1510}},
Month = {{APR 15}},
Abstract = {{An atmospheric general circulation model (AGCM) is forced with a
   prescribed SST dipole anomaly in the tropical Atlantic to investigate
   the cause of crossequatorial SST gradient (CESG) variability and its
   teleconnection tb the extratropics. The model response bears a striking
   resemblance to observations in both the tropics and extratropics. The
   tropical response is robust and can act to reinforce the prescribed SST
   anomalies through wind-induced evaporation. A new feedback mechanism
   involving low-level stratiform clouds in the subtropics is also
   identified in the model and observations. The tropical SST dipole forces
   a barotropic teleconnection into the extratropics that projects onto the
   North Atlantic Oscillation (NAO). It further induces the extratropical
   portion of the North Atlantic SST tripole when the AGCM is coupled with
   an ocean mixed layer model. CESG variability thus appears to be the
   centerpiece of a pan-Atlantic climate pattern observed to extend from
   the South Atlantic to Greenland.}},
Publisher = {{AMER GEOPHYSICAL UNION}},
Address = {{2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Okumura, Y (Corresponding Author), Univ Hawaii Manoa, Dept Meteorol, 2525 Correa Rd, Honolulu, HI 96822 USA.
   Univ Hawaii Manoa, Dept Meteorol, Honolulu, HI 96822 USA.
   Hokkaido Univ, Grad Sch Environm Earth Sci, Sapporo, Hokkaido 0600810, Japan.}},
DOI = {{10.1029/2000GL012565}},
ISSN = {{0094-8276}},
Keywords-Plus = {{SURFACE TEMPERATURE; CLIMATE VARIABILITY; OCEAN; NORTH; CIRCULATION;
   OSCILLATION; MIDLATITUDE; RAINFALL}},
Research-Areas = {{Geology}},
Web-of-Science-Categories  = {{Geosciences, Multidisciplinary}},
ResearcherID-Numbers = {{Okumura, Yuko/A-9742-2012
   Tanimoto, Youichi/F-8819-2012
   Xie, Shang-Ping/C-1254-2009}},
ORCID-Numbers = {{Xie, Shang-Ping/0000-0002-3676-1325}},
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Number-of-Cited-References = {{23}},
Times-Cited = {{109}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{3}},
Journal-ISO = {{Geophys. Res. Lett.}},
Doc-Delivery-Number = {{421LP}},
Unique-ID = {{ISI:000168066100026}},
OA = {{Green Published}},
DA = {{2020-08-06}},
}

@article{ ISI:000168066100029,
Author = {Rodionov, S and Assel, R},
Title = {{A new look at the Pacific/North American index}},
Journal = {{GEOPHYSICAL RESEARCH LETTERS}},
Year = {{2001}},
Volume = {{28}},
Number = {{8}},
Pages = {{1519-1522}},
Month = {{APR 15}},
Abstract = {{This study examines inconsistencies in the Pacific/North American (PNA)
   index relative to atmospheric circulation over North America. Two types
   of atmospheric circulation were found to be associated with high PNA
   values. The first type is the true PNA pattern characterized by an
   amplified ridge-trough system. It appears to be related to the leading
   mode of sea surface temperature variability in the North Pacific. The
   second type is observed during El Nino events. It is characterized by a
   flattening of the polar jet stream and southward shift of the
   subtropical jet stream. The recognition of these two types of the PNA
   index improves our understanding of the relative role of to El
   Nino/Southern Oscillation events and sea surface temperatures in the
   North Pacific in affecting winter atmospheric circulation over North
   America.}},
Publisher = {{AMER GEOPHYSICAL UNION}},
Address = {{2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Rodionov, S (Corresponding Author), Univ Colorado, Dept Comp Sci, Campus Box 430, Boulder, CO 80309 USA.
   NOAA, Great Lakes Environm Res Lab, Ann Arbor, MI 48105 USA.}},
DOI = {{10.1029/2000GL012185}},
ISSN = {{0094-8276}},
Keywords-Plus = {{UNITED-STATES CLIMATE; TELECONNECTION PATTERN; CIRCULATION PATTERNS;
   VARIABILITY; ENSO; WINTER; OSCILLATION}},
Research-Areas = {{Geology}},
Web-of-Science-Categories  = {{Geosciences, Multidisciplinary}},
ORCID-Numbers = {{Rodionov, Sergei/0000-0002-5318-9746}},
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Number-of-Cited-References = {{18}},
Times-Cited = {{23}},
Usage-Count-Last-180-days = {{2}},
Usage-Count-Since-2013 = {{9}},
Journal-ISO = {{Geophys. Res. Lett.}},
Doc-Delivery-Number = {{421LP}},
Unique-ID = {{ISI:000168066100029}},
DA = {{2020-08-06}},
}

@article{ ISI:000168066100032,
Author = {Jin, FF and Kimoto, M and Wang, XC},
Title = {{A model of decadal ocean-atmosphere interaction in the North Pacific
   basin}},
Journal = {{GEOPHYSICAL RESEARCH LETTERS}},
Year = {{2001}},
Volume = {{28}},
Number = {{8}},
Pages = {{1531-1534}},
Month = {{APR 15}},
Abstract = {{From a simple and a global coupled model, we showed that the tropical
   and extratropical ocean-atmosphere interactions and the teleconnection
   between the tropics and extratropics in these interactions are
   responsible for the co-variations of the decadal to interdecadal climate
   fluctuations in the tropical and extratropical Pacific. The subtropical
   oceanic Rossby waves are found to play an important role in forming the
   coupled decadal to interdecadal mode. They are responsible for slow
   exchanges of mass and heat between the tropical and subtropical ocean
   gyres that serve as an important oceanic linking bridge of the tropical
   and extratropical decadal to interdecadal ocean-atmosphere interactions
   in the Pacific basin.}},
Publisher = {{AMER GEOPHYSICAL UNION}},
Address = {{2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Jin, FF (Corresponding Author), Univ Hawaii Manoa, Dept Meteorol, 2525 Correa Rd, Honolulu, HI 96822 USA.
   Univ Hawaii Manoa, Dept Meteorol, Honolulu, HI 96822 USA.
   Univ Tokyo, Ctr Climate Syst Res, Meguro Ku, Tokyo 153, Japan.}},
DOI = {{10.1029/2000GL008478}},
ISSN = {{0094-8276}},
Keywords-Plus = {{CLIMATE VARIABILITY; ENSO}},
Research-Areas = {{Geology}},
Web-of-Science-Categories  = {{Geosciences, Multidisciplinary}},
ResearcherID-Numbers = {{kimoto, masahide/P-9077-2014}},
Cited-References = {{Gu DF, 1997, SCIENCE, V275, P805, DOI 10.1126/science.275.5301.805.
   Jin FF, 1997, J CLIMATE, V10, P1821, DOI 10.1175/1520-0442(1997)010<1821:ATOICV>2.0.CO;2.
   Jin FF, 1997, J ATMOS SCI, V54, P811, DOI 10.1175/1520-0469(1997)054<0811:AEORPF>2.0.CO;2.
   LATIF M, 1994, SCIENCE, V266, P634, DOI 10.1126/science.266.5185.634.
   Lysne J, 1997, GEOPHYS RES LETT, V24, P2589, DOI 10.1029/97GL02751.
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   Zhang Y, 1997, J CLIMATE, V10, P1004, DOI 10.1175/1520-0442(1997)010<1004:ELIV>2.0.CO;2.}},
Number-of-Cited-References = {{9}},
Times-Cited = {{15}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{5}},
Journal-ISO = {{Geophys. Res. Lett.}},
Doc-Delivery-Number = {{421LP}},
Unique-ID = {{ISI:000168066100032}},
DA = {{2020-08-06}},
}

@article{ ISI:000168698400010,
Author = {Mohanty, UC and Niyogi, DS and Raman, S and Sarkar, A},
Title = {{Numerical study of the role of land-air-sea interactions for the
   northeasterly monsoon circulations over Indian Ocean during INDOEX}},
Journal = {{CURRENT SCIENCE}},
Year = {{2001}},
Volume = {{80}},
Number = {{S}},
Pages = {{60-68}},
Month = {{APR 10}},
Abstract = {{One of the principal objectives of the Indian Ocean Experiment (INDOEX)
   was to study the aerosol transport from the Indian subcontinent to the
   pristine oceanic environment. The underlying hypothesis for INDOEX is
   that, during the northeasterly monsoon, the intruding aerosols and other
   anthropogenic pollutants can entrain into the Inter Tropical Convergence
   Zone (ITCZ) and the Equatorial Indian Ocean and finally into the clouds,
   The altered clouds influence the radiative transfer processes at the
   regional and possibly global scale. The driving mechanism for the
   regional transport was the boundary layer circulation. In this study, it
   was hypothesized that the circulation pattern, which affects the
   regional transport, was strongly influenced by the land-air-sea
   interactions. To test this, a zonally symmetric version of a primitive
   equation numerical weather prediction model, called the Advanced
   Regional Prediction System (ARPS), was used. A number of numerical
   experiments were performed for a 2-D domain ranging from 14 degreesN to
   16 degreesS centered over 76 degreesE, In the experiments, the influence
   of land-sea interaction (differential heating), topography (Western
   Chats), and the thermal gradients (SST and land surface temperature) on
   the coastal circulations over Equatorial Indian Ocean were studied.
   Results indicated a strong land-air-sea interaction and feedback
   teleconnection between the local and large scale features.
   Interestingly, the model generated land influence to the order of 1000
   km offshore in the simulation domain, consistent with different
   observations. Results suggest that the oceanic environment in the
   northeast monsoon over Arabian Sea and the Indian Ocean can display
   significant diurnal variability and heterogeneity due to topography and
   surface temperature gradients, and that the local features have
   interactive feedback on the large scale circulations and transport.}},
Publisher = {{CURRENT SCIENCE ASSN}},
Address = {{C V RAMAN AVENUE, PO BOX 8005, BANGALORE 560 080, INDIA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Mohanty, UC (Corresponding Author), Indian Inst Technol, Ctr Atmospher Sci, Hauz Khas, New Delhi 110016, India.
   Indian Inst Technol, Ctr Atmospher Sci, New Delhi 110016, India.
   N Carolina State Univ, State Climate Off NC, Raleigh, NC 27695 USA.
   N Carolina State Univ, Dept Marine Earth \& Atmospher Sci, Raleigh, NC 27695 USA.}},
ISSN = {{0011-3891}},
Keywords-Plus = {{BOUNDARY-LAYER; SIMULATION; AEROSOL; CRUISE}},
Research-Areas = {{Science \& Technology - Other Topics}},
Web-of-Science-Categories  = {{Multidisciplinary Sciences}},
Cited-References = {{HONG X, 1994, ATMOS ENVIRON, V29, P2163.
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Number-of-Cited-References = {{15}},
Times-Cited = {{4}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{2}},
Journal-ISO = {{Curr. Sci.}},
Doc-Delivery-Number = {{432NR}},
Unique-ID = {{ISI:000168698400010}},
DA = {{2020-08-06}},
}

@article{ ISI:000169375900010,
Author = {Franzke, C and Fraedrich, K and Lunkeit, F},
Title = {{Teleconnections and low-frequency variability in idealized experiments
   with two storm tracks}},
Journal = {{QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY}},
Year = {{2001}},
Volume = {{127}},
Number = {{574, B}},
Pages = {{1321-1339}},
Month = {{APR}},
Abstract = {{Low-frequency variability and teleconnection patterns induced by two
   storm tracks in idealized experiments depend on their zonal distance. A
   separation of about 150 degrees, which resembles the northern hemisphere
   storm-track distribution, reveals teleconnection patterns which are
   similar to the Pacific North American (PNA) pattern and the North
   Atlantic Oscillation (NAO). The NAG-like structure is associated with
   retrograde travelling Rossby waves: barotropic stream-function
   tendencies show that the interaction of the stationary eddies with the
   low-frequency how and the high-frequency eddies contribute to the
   amplification of the pattern. Its decay is due to their interaction with
   the zonal-mean flow, and the low-frequency contribution to the
   divergence term. The PNA-like pattern has a longer memory and is linked
   to a quasi-stationary wave. The stationary-wave activity flux shows the
   dominating influence of baroclinic processes and the other storm track
   further upstream. The correlation between the teleconnection indices is
   significant for storm-track distances between 180 degrees and 160
   degrees, and vanishes between 150 degrees and 130 degrees.}},
Publisher = {{WILEY-BLACKWELL}},
Address = {{111 RIVER ST, HOBOKEN 07030-5774, NJ USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Fraedrich, K (Corresponding Author), Univ Hamburg, Inst Meteorol, Bundesstr 55, D-20146 Hamburg, Germany.
   Univ Hamburg, Inst Meteorol, D-20146 Hamburg, Germany.}},
DOI = {{10.1002/qj.49712757411}},
ISSN = {{0035-9009}},
EISSN = {{1477-870X}},
Keywords = {{idealized experiments; low-frequency variability; storm-track
   interaction; teleconnection}},
Keywords-Plus = {{GLOBAL CIRCULATION MODEL; 500-MB HEIGHT FLUCTUATIONS; NORTH
   PACIFIC-OCEAN; SHORT-TIME SCALES; GEOPOTENTIAL HEIGHT; STATIONARY WAVES;
   LIFE-CYCLES; HEMISPHERE; ANOMALIES; FLOW}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{fraedrich@dkrz.de}},
ResearcherID-Numbers = {{Franzke, Christian L E/A-6191-2012}},
ORCID-Numbers = {{Franzke, Christian L E/0000-0003-4111-1228}},
Cited-References = {{BLACK RX, 1993, J ATMOS SCI, V50, P421, DOI 10.1175/1520-0469(1993)050<0421:TDOLSC>2.0.CO;2.
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Number-of-Cited-References = {{33}},
Times-Cited = {{16}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{6}},
Journal-ISO = {{Q. J. R. Meteorol. Soc.}},
Doc-Delivery-Number = {{444AN}},
Unique-ID = {{ISI:000169375900010}},
DA = {{2020-08-06}},
}

@article{ ISI:000168712500002,
Author = {Saenz, J and Zubillaga, J and Rodriguez-Puebla, C},
Title = {{Interannual winter temperature variability in the north of the Iberian
   Peninsula}},
Journal = {{CLIMATE RESEARCH}},
Year = {{2001}},
Volume = {{16}},
Number = {{3}},
Pages = {{169-179}},
Month = {{MAR 21}},
Abstract = {{This work analyses the interannual variability of winter temperature in
   the north of the Iberian Peninsula, This area exhibits a different
   behaviour to the rest of the Iberian Peninsula, according to the loading
   factors of the leading empirical orthogonal function of Iberian winter
   temperature and precipitation. The regional time series is defined by
   means of principal components analysis (PCA) as a data reduction tool.
   The only significant eigenvalue can be related to synoptic causes. It is
   linked, for signals with a period lower than 10 yr, to the East Atlantic
   teleconnection pattern. It does not show any significant correlation to
   the North Atlanic Oscillation (NAO) or Arctic Oscillation (AO), which
   are the major factors controlling temperature over European or Iberian
   areas. This result agrees with previously published works and can be
   explained on the basis of enthalpy transport density vectors and
   geopotential anomaly over the area. Eddy terms do not play a significant
   role in this relationship. The link of the interannual variability of
   temperature in the area with the Atlantic sea surface temperature (SST)
   is also analysed, but SSTs do not show any significant predictive skill,
   and the statistically significant relationship does not seem to be
   causal.}},
Publisher = {{INTER-RESEARCH}},
Address = {{NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Saenz, J (Corresponding Author), Univ Basque Country, Dept Fis Aplicada 2, Bilbao 46080, Spain.
   Univ Basque Country, Dept Fis Aplicada 2, Bilbao 46080, Spain.
   Univ Basque Country, Dept Fis Mat Condensada, Bilbao 46080, Spain.
   Univ Salamanca, Dept Fis Atmosfera, E-37008 Salamanca, Spain.}},
DOI = {{10.3354/cr016169}},
ISSN = {{0936-577X}},
EISSN = {{1616-1572}},
Keywords = {{cantabrian; Iberian; winter; temperature; variability}},
Keywords-Plus = {{SEA-SURFACE TEMPERATURE; HEAT-FLUX ANOMALIES; ATLANTIC OSCILLATION;
   ATMOSPHERIC CIRCULATION; TIME-SERIES; TROPOSPHERIC TEMPERATURE;
   GEOPOTENTIAL HEIGHT; HEMISPHERE WINTER; HOMOGENEITY TEST; PRECIPITATION}},
Research-Areas = {{Environmental Sciences \& Ecology; Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Environmental Sciences; Meteorology \& Atmospheric Sciences}},
Author-Email = {{wdpsaagj@lg.ehu.es}},
ResearcherID-Numbers = {{Rodriguez-Puebla, Concepcion/C-1414-2011
   Saenz, Jon/A-7500-2011}},
ORCID-Numbers = {{Rodriguez-Puebla, Concepcion/0000-0003-0018-6805
   Saenz, Jon/0000-0002-5920-7570}},
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Number-of-Cited-References = {{55}},
Times-Cited = {{36}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{4}},
Journal-ISO = {{Clim. Res.}},
Doc-Delivery-Number = {{432TV}},
Unique-ID = {{ISI:000168712500002}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000168077200006,
Author = {Vergani, DF and Stanganelli, ZB and Bilenca, D},
Title = {{Weaning mass variation of southern elephant seals at King George Island
   and its possible relationship with ``El Nino{''} and ``La Nina{''}
   Events}},
Journal = {{ANTARCTIC SCIENCE}},
Year = {{2001}},
Volume = {{13}},
Number = {{1}},
Pages = {{37-40}},
Month = {{MAR}},
Abstract = {{Possible effects of ``El Nino{''} Southern Oscillation (ENSO) components
   ``El Nino{''} and ``La Nina{''} on populations of southern elephant
   seals, Mirounga leonina L., are considered in this study. Information on
   pup weaning mass, collected at King George Island, South Shetland
   Islands, over a ten-year period (1985-94) was analysed with respect to
   the occurrence of ENSO and recent research in feeding ecology of this
   population in the Bellinghausen Sea. Weaning mass of elephant seals was
   found to be higher during ``La Nina{''} and a lower during ``El
   Nino{''}. Differences in weaning mass between sexes varied in different
   proportions during El Nino and La Nina. The teleconnection between
   tropical Pacific anomalies and the Bellinghausen Sea deserves further
   research, and our results suggest a way to study this phenomenon using
   data of elephant seal pups weaning mass as indicators of changes in food
   availability.}},
Publisher = {{CAMBRIDGE UNIV PRESS}},
Address = {{110 MIDLAND AVE, PORT CHESTER, NY 10573-4930 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Vergani, DF (Corresponding Author), CONICET, CENPAT, Ctr Nacl Patagon, Blvd Alm Brown 3500, RA-9120 Puerto Madryn, Chubut, Argentina.
   CONICET, CENPAT, Ctr Nacl Patagon, RA-9120 Puerto Madryn, Chubut, Argentina.
   Elephant Seals Project, RA-9120 Puerto Madryn, Chubut, Argentina.
   Univ Buenos Aires, Fac Ciencias Exactas \& Nat, Dept Ciencias Biol, RA-1428 Buenos Aires, DF, Argentina.}},
DOI = {{10.1017/S0954102001000062}},
ISSN = {{0954-1020}},
Keywords = {{El Nino; ENSO; La Nina; Mirounga leonina; southern elephant seals;
   weaning mass}},
Keywords-Plus = {{PUPS}},
Research-Areas = {{Environmental Sciences \& Ecology; Physical Geography; Geology}},
Web-of-Science-Categories  = {{Environmental Sciences; Geography, Physical; Geosciences,
   Multidisciplinary}},
ResearcherID-Numbers = {{Vergani, Daniela/Z-3026-2019
   }},
ORCID-Numbers = {{Vergani, Daniela/0000-0003-0898-2216}},
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Number-of-Cited-References = {{12}},
Times-Cited = {{24}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{3}},
Journal-ISO = {{Antarct. Sci.}},
Doc-Delivery-Number = {{421RK}},
Unique-ID = {{ISI:000168077200006}},
DA = {{2020-08-06}},
}

@article{ ISI:000167232100013,
Author = {Alberghina, L and Porro, D and Cazzador, L},
Title = {{Towards a blueprint of the cell cycle}},
Journal = {{ONCOGENE}},
Year = {{2001}},
Volume = {{20}},
Number = {{9}},
Pages = {{1128-1134}},
Month = {{MAR 1}},
Abstract = {{The understanding of the organisation of cell cycle events is of utmost
   importance. to devise effective therapeutic strategies for cancer, In
   this article we gather evidences from the literature in support of a
   system model of the cell cycle, in which a growth-sensitive threshold
   controls entry into S phase and the sequential activation of
   cyclin-dependent kinases, The cycle is terminated by an End function,
   that comprises events from the onset of mitosis to cell division and
   that may also be modulated by the increase of cell size, This blueprint
   allows quantitative predictions by computer simulations of steady and
   transitory states. In fact, we show that the proposed control system
   applies to budding yeast populations during nutritional shift-up and
   following hyperactivation of the cAMP signalling pathway, Besides the
   growth-sensitive control system it is shown to apply to mammalian cells
   both in the exit from quiescence and in active proliferation, The
   putative molecular determinants that set the threshold controlling S
   phase entry are consistently altered in cancer cells, Finally, we
   discuss an input/output analysis based on the simulated behaviour
   derived from the blueprint as a new tool to investigate the road to
   cancer.}},
Publisher = {{NATURE PUBLISHING GROUP}},
Address = {{HOUNDMILLS, BASINGSTOKE RG21 6XS, HAMPSHIRE, ENGLAND}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Alberghina, L (Corresponding Author), Univ Milan, Biocca, Dept Biosci \& Biotechnol, Pzza Sci 2, I-20126 Milan, Italy.
   Univ Milan, Biocca, Dept Biosci \& Biotechnol, I-20126 Milan, Italy.
   Natl Res Council, Inst Syst Sci \& Biomed Engn, I-35127 Padua, Italy.}},
DOI = {{10.1038/sj.onc.1204263}},
ISSN = {{0950-9232}},
Keywords = {{cell cycle; CDK; CKI; cyclin; budding yeast; cancer}},
Keywords-Plus = {{YEAST SACCHAROMYCES-CEREVISIAE; BUDDING YEAST; G1 CYCLINS;
   FLOW-CYTOMETRY; G2 CYCLINS; GROWTH; G(1); PROGRESSION; PATHWAY; PHASE}},
Research-Areas = {{Biochemistry \& Molecular Biology; Oncology; Cell Biology; Genetics \&
   Heredity}},
Web-of-Science-Categories  = {{Biochemistry \& Molecular Biology; Oncology; Cell Biology; Genetics \&
   Heredity}},
ORCID-Numbers = {{PORRO, DANILO/0000-0001-5723-3700
   Alberghina, Lilia/0000-0003-1694-931X}},
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Number-of-Cited-References = {{44}},
Times-Cited = {{21}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{3}},
Journal-ISO = {{Oncogene}},
Doc-Delivery-Number = {{406TW}},
Unique-ID = {{ISI:000167232100013}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000167003800004,
Author = {Liang, XZ and Wang, WC and Samel, AN},
Title = {{Biases in AMIP model simulations of the east China monsoon system}},
Journal = {{CLIMATE DYNAMICS}},
Year = {{2001}},
Volume = {{17}},
Number = {{4}},
Pages = {{291-304}},
Month = {{FEB}},
Abstract = {{AMIP model simulations of the east China (5-50 degreesN; 105-122
   degreesE) monsoon system are analyzed to study coherent relationships
   between rainfall and wind annual cycle biases. A comparison with
   observed interannual variability patterns is carried out to identify the
   physical processes that explain the biases. The analyses show that
   poleward displacement of the simulated east Asian jet stream causes the
   ascending branch of the jet-induced transverse circulation to move north
   and, as a consequence, produces negative (positive) rainfall biases
   occur in central (northeast) China. The model simulations show decreased
   southwesterly flow and ITCZ rainfall over the South China Sea when
   weaker (versus observations) summer Hadley and Walker circulations are
   present. This results from diminished model tropical disturbance
   activity, and highlights the importance of air-sea interactions. In
   addition, during October-January, intensified model low-level easterlies
   enhance moisture transport and produce positive local rainfall biases
   over central and northeast China. Biases in the east China monsoon
   system are concurrently reflected in the planetary circulation. Enhanced
   northeast China rainfall results from increased surface pressure over
   the North Pacific and an amplified zonal pressure gradient along the
   east China coast. This bias pattern is associated with differences in
   model representations of topography. On the other hand, the South China
   Sea experiences an extensive elongated meridional rainfall bias dipole
   structure that straddles the equator. This is accompanied by a
   baroclinic vertical pattern over the tropics as well as a barotropic
   wave train that extends from Australia to the Antarctic, where the
   teleconnection is likely a direct atmospheric response to tropical
   convective heating.}},
Publisher = {{SPRINGER-VERLAG}},
Address = {{175 FIFTH AVE, NEW YORK, NY 10010 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Liang, XZ (Corresponding Author), Illinois State Water Survey, Dept Nat Resources, 2204 Griffith Dr, Champaign, IL 61820 USA.
   Illinois State Water Survey, Dept Nat Resources, Champaign, IL 61820 USA.
   Univ Illinois, Champaign, IL 61820 USA.
   SUNY Albany, Atmospher Sci Res Ctr, Albany, NY 12222 USA.
   Bowling Green State Univ, Geog Program, Bowling Green, OH 43403 USA.
   Bowling Green State Univ, Environm Program, Bowling Green, OH 43403 USA.}},
DOI = {{10.1007/s003820000136}},
ISSN = {{0930-7575}},
Keywords-Plus = {{GENERAL-CIRCULATION MODEL; COMMUNITY-CLIMATE-MODEL; INTERCOMPARISON
   PROJECT; PRECIPITATION; VARIABILITY; RAINFALL; GCM; ASSOCIATIONS;
   ATMOSPHERE}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
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Number-of-Cited-References = {{28}},
Times-Cited = {{32}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{7}},
Journal-ISO = {{Clim. Dyn.}},
Doc-Delivery-Number = {{402TG}},
Unique-ID = {{ISI:000167003800004}},
DA = {{2020-08-06}},
}

@article{ ISI:000167348600003,
Author = {Esteves, MA and Orgaz, MDM},
Title = {{The influence of climatic variability on the quality of wine}},
Journal = {{INTERNATIONAL JOURNAL OF BIOMETEOROLOGY}},
Year = {{2001}},
Volume = {{45}},
Number = {{1}},
Pages = {{13-21}},
Month = {{FEB}},
Abstract = {{In this paper, the quality of the wine from the Dao (Viseu) region of
   Portugal is examined and relationships between wine quality and climatic
   variability are obtained using spectral and correlation analysis to
   determine the structure of the temporal variations. The spectra of the
   series of quality of wine values show statistically significant
   oscillations coherent with those found in the series of teleconnection
   indices. The series cover a period of 33 years. A significant
   correlation was obtained between wine quality and minimum air
   temperature in May, December and total precipitation in April. The
   teleconnection circulation indices are used to provide some physical
   insight into the most significant oscillating components of the climatic
   and the wine quality series. We found significant and positive
   correlations between the quality of the wine and the Southern
   Oscillation Index (SOI) of August and negative with the SOI of January
   and with the North Atlantic Oscillation of April. Wine quality and
   climatic series can be predicted using statistical models depending on
   significant oscillations.}},
Publisher = {{SPRINGER-VERLAG}},
Address = {{175 FIFTH AVE, NEW YORK, NY 10010 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Orgaz, MDM (Corresponding Author), Univ Aveiro, Dept Phys, P-3800 Aveiro, Portugal.
   Univ Aveiro, Dept Phys, P-3800 Aveiro, Portugal.
   Sup Agrarian Sch, Viseu, Portugal.}},
DOI = {{10.1007/s004840000075}},
ISSN = {{0020-7128}},
Keywords-Plus = {{PRECIPITATION VARIABILITY; ATMOSPHERIC CIRCULATION; TEMPERATURE;
   PORTUGAL; PATTERNS; WINTER}},
Research-Areas = {{Biophysics; Environmental Sciences \& Ecology; Meteorology \&
   Atmospheric Sciences; Physiology}},
Web-of-Science-Categories  = {{Biophysics; Environmental Sciences; Meteorology \& Atmospheric Sciences;
   Physiology}},
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Number-of-Cited-References = {{24}},
Times-Cited = {{19}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{12}},
Journal-ISO = {{Int. J. Biometeorol.}},
Doc-Delivery-Number = {{408VV}},
Unique-ID = {{ISI:000167348600003}},
DA = {{2020-08-06}},
}

@article{ ISI:000166259100044,
Author = {Blunier, T and Brook, EJ},
Title = {{Timing of millennial-scale climate change in Antarctica and Greenland
   during the last glacial period}},
Journal = {{SCIENCE}},
Year = {{2001}},
Volume = {{291}},
Number = {{5501}},
Pages = {{109-112}},
Month = {{JAN 5}},
Abstract = {{A precise relative chronology for Greenland and West Antarctic
   paleotemperature is extended to 90,000 years ago, based on correlation
   of atmospheric methane records from the Greenland Ice Sheet Project 2
   and Byrd ice cores. Over this period, the onset of seven major
   millennial-scale warmings in Antarctica preceded the onset of Greenland
   warmings by 1500 to 3000 years. In general, Antarctic temperatures
   increased gradually while Greenland temperatures were decreasing or
   constant, and the termination of Antarctic warming was apparently
   coincident with the onset of rapid warming in Greenland. This pattern
   provides further evidence for the operation of a ``bipolar see-saw{''}
   in air temperatures and an oceanic teleconnection between the
   hemispheres on millennial time scales.}},
Publisher = {{AMER ASSOC ADVANCEMENT SCIENCE}},
Address = {{1200 NEW YORK AVE, NW, WASHINGTON, DC 20005 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Blunier, T (Corresponding Author), Princeton Univ, Dept Geosci, Guyot Hall, Princeton, NJ 08544 USA.
   Princeton Univ, Dept Geosci, Princeton, NJ 08544 USA.
   Univ Bern, Inst Phys, CH-3012 Bern, Switzerland.
   Washington State Univ, Dept Geol, Vancouver, WA 98686 USA.
   Washington State Univ, Environm Sci Program, Vancouver, WA 98686 USA.}},
DOI = {{10.1126/science.291.5501.109}},
ISSN = {{0036-8075}},
EISSN = {{1095-9203}},
Keywords-Plus = {{ICE CORE; NORTH-ATLANTIC; ISOTOPE; RECORD; DEGLACIATION; TRANSITION;
   PROFILES; STATION; GISP2; CYCLE}},
Research-Areas = {{Science \& Technology - Other Topics}},
Web-of-Science-Categories  = {{Multidisciplinary Sciences}},
Author-Email = {{blunier@princeton.edu}},
ResearcherID-Numbers = {{Blunier, Thomas/M-4609-2014}},
ORCID-Numbers = {{Blunier, Thomas/0000-0002-6065-7747}},
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Number-of-Cited-References = {{33}},
Times-Cited = {{742}},
Usage-Count-Last-180-days = {{9}},
Usage-Count-Since-2013 = {{181}},
Journal-ISO = {{Science}},
Doc-Delivery-Number = {{389VJ}},
Unique-ID = {{ISI:000166259100044}},
DA = {{2020-08-06}},
}

@inproceedings{ ISI:000177601900090,
Author = {Yu, JY and Mechoso, CR},
Book-Group-Author = {{AMS
   AMS}},
Title = {{A Indo-Pacific SST teleconnection pattern during ENSO}},
Booktitle = {{12TH SYMPOSIUM ON GLOBAL CHANGE AND CLIMATE VARIATIONS}},
Year = {{2001}},
Pages = {{293-296}},
Note = {{12th Symposium on Global Change and Climate Variations, ALBUQUERQUE, NM,
   JAN 14-18, 2001}},
Organization = {{Amer Meteorol Soc}},
Publisher = {{AMER METEOROLOGICAL SOCIETY}},
Address = {{45 BEACON ST, BOSTON, MA 02108 USA}},
Type = {{Proceedings Paper}},
Language = {{English}},
Affiliation = {{Yu, JY (Corresponding Author), Univ Calif Los Angeles, Dept Atmospher Sci, 405 Hilgard Ave, Los Angeles, CA 90095 USA.
   Univ Calif Los Angeles, Dept Atmospher Sci, Los Angeles, CA 90095 USA.}},
Keywords-Plus = {{MONSOON}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
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Number-of-Cited-References = {{13}},
Times-Cited = {{1}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{0}},
Doc-Delivery-Number = {{BV01M}},
Unique-ID = {{ISI:000177601900090}},
DA = {{2020-08-06}},
}

@article{ ISI:000171190400005,
Author = {Fang, ZF and Wallace, JM and Thompson, DWJ},
Title = {{The relationship between the meridional profile of zonal-mean
   geostrophic wind and station wave at 500 hPa}},
Journal = {{ADVANCES IN ATMOSPHERIC SCIENCES}},
Year = {{2001}},
Volume = {{18}},
Number = {{5}},
Pages = {{692-700}},
Note = {{International Conference on Climate and Environment Variability and
   Predictability (CEVP), SHANGHAI, PEOPLES R CHINA, AUG 07-11, 2000}},
Organization = {{Atmospher Sci \& Geophys Fluid Dynam, Natl Key Lab; Inst Atmospher Phys;
   Chinese Acad Sci}},
Abstract = {{The sea-level pressure (SLP), 500 hPa height, zonal-mean 500 hPa height
   ({[}Z(500)]), stationary wave eddy component of the 500 hPa height
   (Z(500){*}) and zonal-mean 500 hPa geostrophic wind {[}U-g] fields
   poleward of 20 degreesN are examined for the period 1958-1997, with
   emphasis on the winter season. The relationships between the Arctic
   Oscillation (AO)index and algebraic difference of the zonal-mean wind in
   55 degreesN and 35 degreesN (Ut) index were investigated, making use the
   Monte Carlo procedure, Singular Value Decomposition (SVD), Empirical
   orthogonal function (EOF) and regression method. The leading modes of
   empirical orthogonal function (EOF's) of SLP are more robust than the
   500 hPa height EOF's. not only in the ratio of the two largest
   eigenvalues, but in more zonally symmetric. Comparing the meridional
   profiles of zonal-mean wind amplitude associated with the AO and Ut
   index, the profiles for the two indexes are very similar, both with
   respect to amplitude and the placement of the maximum and minimum.
   Comparing the station wave component of 500 hPa height field regressed
   upon the AO and Ut index. there is one-to-one correspondence between all
   the major centers of action in the two maps, especially in the North
   Atlantic and Eurasian continent. The pattern is unlike the prominent
   teleconnection patterns, they have hemispheric extent and cannot be
   interpreted in term of the individual wavetrains.}},
Publisher = {{CHINA OCEAN PRESS}},
Address = {{INTERNATIONAL DEPT, 8 DA HUI SHI, BEIJING 100081, PEOPLES R CHINA}},
Type = {{Article; Proceedings Paper}},
Language = {{English}},
Affiliation = {{Fang, ZF (Corresponding Author), Chengdu Univ Informat Technol, Chengdu 610041, Peoples R China.
   Chengdu Univ Informat Technol, Chengdu 610041, Peoples R China.
   Univ Washington, Dept Atmospher Sci, Seattle, WA 98195 USA.}},
ISSN = {{0256-1530}},
Keywords = {{meridional profile; station wave; eddy component; zonal-mean geostrophic
   wind; Arctic Oscillation}},
Keywords-Plus = {{CIRCULATION PATTERNS; NORTHERN HEMISPHERE; GEOPOTENTIAL HEIGHT}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Cited-References = {{BARNSTON AG, 1987, MON WEATHER REV, V115, P1083, DOI 10.1175/1520-0493(1987)115<1083:CSAPOL>2.0.CO;2.
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Number-of-Cited-References = {{8}},
Times-Cited = {{0}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{1}},
Journal-ISO = {{Adv. Atmos. Sci.}},
Doc-Delivery-Number = {{475VN}},
Unique-ID = {{ISI:000171190400005}},
DA = {{2020-08-06}},
}

@article{ ISI:000171190400032,
Author = {Zhu, WJ and Sun, ZB and Zhou, B},
Title = {{The impact of Pacific SSTA on the interannual variability of northern
   Pacific storm track during winter}},
Journal = {{ADVANCES IN ATMOSPHERIC SCIENCES}},
Year = {{2001}},
Volume = {{18}},
Number = {{5}},
Pages = {{1029-1042}},
Note = {{International Conference on Climate and Environment Variability and
   Predictability (CEVP), SHANGHAI, PEOPLES R CHINA, AUG 07-11, 2000}},
Organization = {{Atmospher Sci \& Geophys Fluid Dynam, Natl Key Lab; Inst Atmospher Phys;
   Chinese Acad Sci}},
Abstract = {{Investigation is conducted of the interannual variability of the
   northern Pacific storm track and its concurrent association with 500 hPa
   height and Pacific sea surface temperature (SST) during winter. Evidence
   suggests that during the studying period the center of the northern
   winter Pacific storm track experiences substantial interannual
   variability in the variation of its latitude, longitude and intensity.
   Singular value decomposition (SVD) of 15 winter 500 hPa filtered
   geopotential height variance over the storm track with the tropical and
   northern Pacific SST shows that the first coupled mode depicts the
   effect on the track of SSTA over the equatorial central and eastern
   Pacific, while the second one reflects the impact of Kuroshio SSTA on
   the track. Further Composite analysis indicates, moreover, that the SSTA
   over Kuroshio (equatorial central and eastern Pacific) during winter,
   which is relative to WP (PNA) teleconnection response pattern in 500 hPa
   height field, respectively, exerts crucial influence on the interannual
   variability in vigor and meridianal (zonal) displacement of the track
   over its central and western (eastern) part.}},
Publisher = {{CHINA OCEAN PRESS}},
Address = {{INTERNATIONAL DEPT, 8 DA HUI SHI, BEIJING 100081, PEOPLES R CHINA}},
Type = {{Article; Proceedings Paper}},
Language = {{English}},
Affiliation = {{Zhu, WJ (Corresponding Author), Nanjing Inst Meteorol, Nanjing 210044, Peoples R China.
   Nanjing Inst Meteorol, Nanjing 210044, Peoples R China.
   Chinese Acad Sci, Inst Atmospher Phys, LASG, Beijing 100029, Peoples R China.}},
ISSN = {{0256-1530}},
Keywords = {{storm track; interannual variability; SVD analysis; teleconnection
   pattern}},
Keywords-Plus = {{EL-NINO; HEMISPHERE; DYNAMICS; CIRCULATION; TRANSIENTS; HEIGHT}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
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Number-of-Cited-References = {{16}},
Times-Cited = {{2}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{0}},
Journal-ISO = {{Adv. Atmos. Sci.}},
Doc-Delivery-Number = {{475VN}},
Unique-ID = {{ISI:000171190400032}},
DA = {{2020-08-06}},
}

@inproceedings{ ISI:000173446300076,
Author = {Gildor, H and Tziperman, E},
Editor = {{Jeffries, MO and Eicken, H}},
Title = {{Sea ice, as the glacial cycles' climate switch, and interhemispheric
   thermohaline teleconnections}},
Booktitle = {{ANNALS OF GLACIOLOGY, VOL 33}},
Series = {{ANNALS OF GLACIOLOGY}},
Year = {{2001}},
Volume = {{33}},
Pages = {{501-506}},
Note = {{International-Glaciological-Society Symposium on Sea Ice and Its
   Interactions with the Ocean, Atmosphere and Biosphere, UNIV ALASKA
   FAIRBANKS, FAIRBANKS, ALASKA, JUN 19-23, 2000}},
Organization = {{Arct Res Consortium US; Frontier Res Syst Global Change; US Natl
   Aeronaut \& Space Adm; US Natl Sci Fdn; US Off Naval Res; Amer Geophys
   Union; Int Arct Sci Comm; Int Assoc Phys Sci Ocean, Sea Ice Commiss; Int
   Commiss Snow \& Ice; Japanese Soc Snow \& Ice; Sci Comm Antarct Res}},
Abstract = {{A box model combining the different physical components of the coupled
   ocean, atmosphere, sea-ice and land-ice climate system is used to study
   the possible role of sea ice in the glacial-interglacial oscillations.
   In this paper we investigate the teleconnection between the two
   hemispheres, and suggest a mechanism which can explain the observed
   Southern Ocean sea-ice variability during glacial-interglacial cycles.
   The teleconnection mechanism involves changes in the temperature of the
   water transported from the Northern to the Southern Hemisphere by the
   thermohaline circulation (THC), rather than the amplitude of the THC as
   has often been suggested. The sequence of events proposed by this model
   indicates that it would be especially interesting to obtain accurate
   information on the relative timing of sea-ice and land-ice variations.
   Fuller general circulation models and new sea-ice proxy data are needed
   to quantify the relative role of the proposed teleconnection mechanism.}},
Publisher = {{INT GLACIOLOGICAL SOC}},
Address = {{LENSFIELD RD, CAMBRIDGE CB2 1ER, ENGLAND}},
Type = {{Article; Proceedings Paper}},
Language = {{English}},
Affiliation = {{Gildor, H (Corresponding Author), Weizmann Inst Sci, IL-76100 Rehovot, Israel.
   Weizmann Inst Sci, IL-76100 Rehovot, Israel.}},
DOI = {{10.3189/172756401781818310}},
ISSN = {{0260-3055}},
ISBN = {{0-946417-28-8}},
Keywords-Plus = {{NORTH-ATLANTIC; ANTARCTIC ICE; SHEET; MODEL; OCEAN; CORE; GREENLAND;
   RADIATION; RECORD; AGE}},
Research-Areas = {{Geology}},
Web-of-Science-Categories  = {{Geosciences, Multidisciplinary}},
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