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Number-of-Cited-References = {{59}},
Times-Cited = {{24}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{1}},
Journal-ISO = {{J. Meteorol. Soc. Jpn.}},
Doc-Delivery-Number = {{560ZL}},
Unique-ID = {{ISI:000176111200006}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000172206600002,
Author = {Oosterhaven, J and Eding, GJ and Stelder, D},
Title = {{Clusters, linkages and interregional spillovers: Methodology and policy
   implications for the two Dutch mainports and the rural North}},
Journal = {{REGIONAL STUDIES}},
Year = {{2001}},
Volume = {{35}},
Number = {{9}},
Pages = {{809-822}},
Month = {{DEC}},
Abstract = {{This paper develops a consistent framework to detect regional clusters
   of interrelated economic activity, and to evaluate both the regional and
   the national economic significance of individual sectors and regions. By
   using bi-regional input-output data it appears to be possible to
   distinguish systematically between intraregional clusters and linkages,
   and their interregional spillovers. The methodology is applied to three
   Dutch regions that are especially important from a spatial policy
   perspective. The conclusions, surprisingly, do not substantiate some of
   the traditional beliefs held, especially as regards the assumed
   importance of the Dutch transport sector.}},
Publisher = {{CARFAX PUBLISHING}},
Address = {{RANKINE RD, BASINGSTOKE RG24 8PR, HANTS, ENGLAND}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Oosterhaven, J (Corresponding Author), Univ Groningen, Postbus 800, NL-9700 AV Groningen, Netherlands.
   Univ Groningen, NL-9700 AV Groningen, Netherlands.
   Cent Bur Stat, NL-2270 JM Voorburg, Netherlands.}},
DOI = {{10.1080/00343400120090239}},
ISSN = {{0034-3404}},
Keywords = {{cluster analysis; input-output analysis; transport sector; The
   Netherlands}},
Keywords-Plus = {{REGIONAL POLICY; FRAMEWORK}},
Research-Areas = {{Business \& Economics; Environmental Sciences \& Ecology; Geography;
   Public Administration}},
Web-of-Science-Categories  = {{Economics; Environmental Studies; Geography; Regional \& Urban Planning}},
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Number-of-Cited-References = {{38}},
Times-Cited = {{34}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{10}},
Journal-ISO = {{Reg. Stud.}},
Doc-Delivery-Number = {{493DK}},
Unique-ID = {{ISI:000172206600002}},
DA = {{2020-08-06}},
}

@article{ ISI:000171974000003,
Author = {Fischer, H},
Title = {{Imprint of large-scale atmospheric transport patterns on sea-salt
   records in northern Greenland ice cores}},
Journal = {{JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES}},
Year = {{2001}},
Volume = {{106}},
Number = {{D20}},
Pages = {{23977-23984}},
Month = {{OCT 27}},
Abstract = {{The decadal to interannual variability of sea-salt aerosol
   concentrations in northern Greenland ice cores is investigated and
   contrasted to meteorological reanalysis data over the time span
   1959-1993. Correlation analysis with average data on sea level pressure
   and geopotential height at the 500 mbar level identifies the eastern and
   northeastern Pacific region as the most important center of action
   responsible for variations in sea-salt aerosol export onto the Greenland
   ice sheet which is related to the Pacific/North American teleconnection
   pattern. The Atlantic region, however, appears to be of secondary
   importance only. Correlation coefficients are highest during the first
   quarter of the year but also significant for annual pressure data,
   explaining similar to 20\% of the sea-salt variance in the ice cores.
   Furthermore, higher storm activity in the Pacific center of action, as
   well as in the northern Atlantic, leads to,higher sea-salt
   concentrations in northern Greenland, explaining about 40\% and 17\% of
   the ice core variance. A. 30\% increase during the nineteenth century in
   a 600 year sea-salt record from northeastern Greenland may be
   interpreted, at least in part, as an enhancement of sea-salt export from
   the Pacific region during that time.}},
Publisher = {{AMER GEOPHYSICAL UNION}},
Address = {{2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Fischer, H (Corresponding Author), Alfred Wegener Inst Polar \& Marine Res, Columbusstr, D-27568 Bremerhaven, Germany.
   Alfred Wegener Inst Polar \& Marine Res, D-27568 Bremerhaven, Germany.}},
DOI = {{10.1029/2000JD000175}},
ISSN = {{2169-897X}},
Keywords-Plus = {{NITRATE FIRN CONCENTRATIONS; ATLANTIC OSCILLATION; GEOPOTENTIAL HEIGHT;
   SEASONAL-VARIATIONS; DEPOSITION CHANGES; CLIMATE; SNOW; CIRCULATION;
   ANTARCTICA; SULFATE}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{hufischer@awi-bremerhaven.de}},
ResearcherID-Numbers = {{Fischer, Hubertus/A-1211-2014}},
ORCID-Numbers = {{Fischer, Hubertus/0000-0002-2787-4221}},
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Number-of-Cited-References = {{43}},
Times-Cited = {{21}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{6}},
Journal-ISO = {{J. Geophys. Res.-Atmos.}},
Doc-Delivery-Number = {{489CG}},
Unique-ID = {{ISI:000171974000003}},
OA = {{Green Published}},
DA = {{2020-08-06}},
}

@article{ ISI:000171588000032,
Author = {Pan, JY and Yan, XH and Zheng, Q and Liu, WT},
Title = {{Vector empirical orthogonal function modes of the ocean surface wind
   variability derived from satellite scatterometer data}},
Journal = {{GEOPHYSICAL RESEARCH LETTERS}},
Year = {{2001}},
Volume = {{28}},
Number = {{20}},
Pages = {{3951-3954}},
Month = {{OCT 15}},
Abstract = {{Ocean surface winds derived from NSCAT, QuikSCAT and ERS-1/2
   scatterometer observations during a period from January 1992 to April
   2000 were analyzed using the vector empirical orthogonal function (VEOF)
   method. With the boreal winter and summer oscillation, the first VEOF is
   dominated by the Indian and East Asian monsoons and also shows an annual
   cycle of the trade winds. The second VEOF represents the boreal autumn
   and spring oscillation, and reveals a transition state between winter
   and summer. The third VEOF indicates the wind variability associated
   with El Nino Southern Oscillation (ENSO) events, because the temporal
   mode has a high correlation coefficient of 0.8 with the Southern
   Oscillation Index (SOI). Further more, the third mode reveals the
   teleconnection of the Indian monsoon and wind variability over high
   latitude oceans', such as the Aleutian Low system, with ENSO events.}},
Publisher = {{AMER GEOPHYSICAL UNION}},
Address = {{2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Yan, XH (Corresponding Author), Univ Delaware, Grad Coll Marine Studies, Newark, DE 19716 USA.
   Univ Delaware, Grad Coll Marine Studies, Newark, DE 19716 USA.
   CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA.
   Ocean Univ Qingdao, Ocean Remote Sensing Inst, Qingdao 266003, Peoples R China.}},
DOI = {{10.1029/2001GL013060}},
ISSN = {{0094-8276}},
Keywords-Plus = {{SOUTHERN OSCILLATION; PACIFIC; GCM}},
Research-Areas = {{Geology}},
Web-of-Science-Categories  = {{Geosciences, Multidisciplinary}},
ResearcherID-Numbers = {{Zheng, Quanan/F-9025-2010}},
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Number-of-Cited-References = {{11}},
Times-Cited = {{8}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{2}},
Journal-ISO = {{Geophys. Res. Lett.}},
Doc-Delivery-Number = {{482RA}},
Unique-ID = {{ISI:000171588000032}},
DA = {{2020-08-06}},
}

@article{ ISI:000171468300009,
Author = {Luo, JJ and Yamagata, T},
Title = {{Long-term El Nino-Southern Oscillation (ENSO)-like variation with
   special emphasis on the South Pacific}},
Journal = {{JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS}},
Year = {{2001}},
Volume = {{106}},
Number = {{C10}},
Pages = {{22211-22227}},
Month = {{OCT 15}},
Abstract = {{Mechanisms for El Nino-Southern Oscillation (ENSO)-like decadal (7-35
   years) variability are analyzed using observational data. When a decadal
   positive temperature anomaly occurs in the eastern tropical Pacific, the
   atmospheric response excites negative wind stress curl in the western
   tropical South Pacific, which causes the thermocline to shoal and induce
   a negative temperature anomaly there. The cold anomaly moves
   northwestward to the western and central equatorial region and then
   turns eastward along the equator to reverse the original temperature
   anomaly in the east. The eastward propagation of the oceanic signal
   along the equatorial thermocline correlates with a zonal wind anomaly.
   The cold anomaly in the east grows through tropical air-sea interaction
   and induces a positive wind stress curl, in the western tropical South
   Pacific associated with the atmospheric teleconnection in the Southern
   Hemisphere. Subsequent evolution of the negative phase is similar to
   that of the positive phase. The complete scenario for this ENSO-like
   decadal variability due to the air-sea interaction processes within the
   tropics has a period of similar to 14 years. We also discuss ENSO-like
   variation on the interdecadal (> 35 years) timescale, with possible
   relationship to the 1976-1977 climate regime shift.}},
Publisher = {{AMER GEOPHYSICAL UNION}},
Address = {{2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Luo, JJ (Corresponding Author), Frontier Res Syst Global Change, Inst Global Change Res, Kanazawa Ku, 3173-25 Showa Machi, Yokohama, Kanagawa 2360001, Japan.
   Frontier Res Syst Global Change, Inst Global Change Res, Kanazawa Ku, Yokohama, Kanagawa 2360001, Japan.
   Univ Tokyo, Grad Sch Sci, Dept Earth \& Planetary Sci, Tokyo 1130033, Japan.}},
DOI = {{10.1029/2000JC000471}},
ISSN = {{0148-0227}},
Keywords-Plus = {{NORTH PACIFIC; DECADAL VARIABILITY; CLIMATE VARIABILITY;
   SURFACE-TEMPERATURE; SST ANOMALIES; OCEAN; ENSO; MODEL; TROPICS;
   CIRCULATION}},
Research-Areas = {{Oceanography}},
Web-of-Science-Categories  = {{Oceanography}},
Author-Email = {{luo@jamstec.go.jp
   yamagata@eps.s.u-tokyo.ac.jp}},
ResearcherID-Numbers = {{Luo, Jing-Jia/T-9612-2019
   Luo, Jing-Jia/B-2481-2008
   Yamagata, Toshio/A-1807-2009}},
ORCID-Numbers = {{Luo, Jing-Jia/0000-0003-2181-0638
   Luo, Jing-Jia/0000-0003-2181-0638
   }},
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Number-of-Cited-References = {{37}},
Times-Cited = {{95}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{9}},
Journal-ISO = {{J. Geophys. Res.-Oceans}},
Doc-Delivery-Number = {{480NR}},
Unique-ID = {{ISI:000171468300009}},
DA = {{2020-08-06}},
}

@article{ ISI:000172758400004,
Author = {Rohli, RV and Vega, AJ and Binkley, MR and Britton, SD and Heckman, HE
   and Jenkins, JM and Ono, Y and Sheeler, DE},
Title = {{Synoptic circulation and stream discharge in the Great Lakes basin, USA}},
Journal = {{APPLIED GEOGRAPHY}},
Year = {{2001}},
Volume = {{21}},
Number = {{4}},
Pages = {{369-385}},
Month = {{OCT}},
Abstract = {{Impacts on water resources caused by human activity, natural climate
   variation and longterm climate change are unclear in the US Great Lakes
   region. Improved understanding of the impact of atmospheric circulation
   on stream discharge variability into the Lakes is thus important. In
   this analysis, monthly surface and mid-tropospheric circulation patterns
   suggest that surface pressure variations over Missouri and Illinois are
   most strongly correlated to disc charge. The mid-tropospheric patterns
   most directly related to discharge place the Great Lakes in a
   trough-to-ridge flow pattern. The analysis confirms that at this scale,
   lee shore advection resulting in `lake-effect' precipitation is not very
   important to regional discharge, and neither are variations in the
   Pacific-North American teleconnection. (C) 2001 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 = {{Rohli, RV (Corresponding Author), Louisiana State Univ, Dept Geog \& Anthropol, Baton Rouge, LA 70803 USA.
   Louisiana State Univ, Dept Geog \& Anthropol, Baton Rouge, LA 70803 USA.
   Clarion Univ Pennsylvania, Dept Anthropol Geog \& Earth Sci, Clarion, PA 16214 USA.
   Kent State Univ, Dept Geog, Kent, OH 44242 USA.}},
DOI = {{10.1016/S0143-6228(01)00011-X}},
ISSN = {{0143-6228}},
Keywords = {{atmospheric circulation variability; Great Lakes; precipitation; stream
   discharge}},
Keywords-Plus = {{AMERICAN TELECONNECTION PATTERN; NORTHERN HEMISPHERE WINTER; SOUTHERN
   OSCILLATION; ATMOSPHERIC TELECONNECTIONS; UNITED-STATES; HEIGHT FIELD;
   CLIMATE; PRECIPITATION; FLUCTUATIONS; TEMPERATURE}},
Research-Areas = {{Geography}},
Web-of-Science-Categories  = {{Geography}},
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Number-of-Cited-References = {{33}},
Times-Cited = {{4}},
Usage-Count-Last-180-days = {{2}},
Usage-Count-Since-2013 = {{9}},
Journal-ISO = {{Appl. Geogr.}},
Doc-Delivery-Number = {{502TG}},
Unique-ID = {{ISI:000172758400004}},
DA = {{2020-08-06}},
}

@article{ ISI:000170605400001,
Author = {Bifulco, R and Bretschneider, S},
Title = {{Estimating school efficiency - A comparison of methods using simulated
   data}},
Journal = {{ECONOMICS OF EDUCATION REVIEW}},
Year = {{2001}},
Volume = {{20}},
Number = {{5}},
Pages = {{417-429}},
Month = {{OCT}},
Abstract = {{Developing measures of school performance is crucial for
   performance-based school reform efforts. One approach to developing such
   measures is to apply econometric and linear programming techniques that
   have been developed to measure productive efficiency. This study uses
   simulated data to assess the adequacy of two such methods, Data
   Envelopment Analysis (DEA) and Corrected Ordinary Least Squares (COLS),
   for the purposes of performance-based school reform. Our results suggest
   that in complex data sets typical of education contexts simple versions
   of DEA and COLS do not provide adequate measures of efficiency. In data
   sets simulated to contain both measurement error and endogeneity, rank
   correlations between efficiency estimates and true efficiency values
   range from 0.104 to 0.240. In none of these data sets were either DEA
   and COLS able to place more than 31\% of schools in their true
   performance quintile. (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 = {{Bifulco, R (Corresponding Author), Syracuse Univ, Maxwell Sch Citizenship \& Publ Affairs, Ctr Policy Res, 426 Eggers Hall, Syracuse, NY 13244 USA.
   Syracuse Univ, Maxwell Sch Citizenship \& Publ Affairs, Ctr Policy Res, Syracuse, NY 13244 USA.
   Syracuse Univ, Maxwell Sch Citizenship \& Publ Affairs, Ctr Technol \& Informat Policy, Syracuse, NY 13244 USA.}},
DOI = {{10.1016/S0272-7757(00)00025-X}},
ISSN = {{0272-7757}},
Keywords = {{efficiency; productivity; input output analysis; educational economics;
   educational finance}},
Keywords-Plus = {{DATA ENVELOPMENT ANALYSIS; FRONTIER PRODUCTION FUNCTION; TECHNICAL
   EFFICIENCY; PERFORMANCE; DEA}},
Research-Areas = {{Business \& Economics; Education \& Educational Research}},
Web-of-Science-Categories  = {{Economics; Education \& Educational Research}},
Cited-References = {{Aigner D., 1977, J ECONOMETRICS, V6, P21, DOI DOI 10.1016/0304-4076(77)90052-5.
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Number-of-Cited-References = {{40}},
Times-Cited = {{27}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{17}},
Journal-ISO = {{Econ. Educ. Rev.}},
Doc-Delivery-Number = {{465TE}},
Unique-ID = {{ISI:000170605400001}},
DA = {{2020-08-06}},
}

@article{ ISI:000171932300003,
Author = {Moron, V and Ward, MN and Navarra, A},
Title = {{Observed and SST-forced seasonal rainfall variability across tropical
   America}},
Journal = {{INTERNATIONAL JOURNAL OF CLIMATOLOGY}},
Year = {{2001}},
Volume = {{21}},
Number = {{12}},
Pages = {{1467-1501}},
Month = {{OCT}},
Abstract = {{Three experiments starting from different initial conditions have been
   made with the ECHAM-4 atmospheric General Circulation Model (GCM)
   integrated at T30 resolution forced with the observed sea-surface
   temperature (SST) over the period 1960-1994. The tropical America modes
   of seasonal rainfall anomalies whose time variation is most accurately
   simulated by the GCM have been searched for using Singular Value
   Decomposition Analyses (SVDA) and Canonical Correlation Analysis (CCA)
   between observed and model fields. The leading modes revealed by SVDA
   and CCA are highly similar, even though the ordering of the modes showed
   some fluctuation. A first skilful rainfall anomaly mode has weights of
   the same sign almost everywhere in tropical America. except along the
   western coast and the sub-tropical margins. This mode appears in all of
   the four seasons assessed. A second major skilful mode is usually a
   bipolar north-south (N-S) rainfall anomaly pattern (clear in
   December-March, DJFM: March-May, MAM, and June-September. JJAS).
   A large portion of the skill of the first rainfall anomaly mode (same
   sign anomalies across tropical America except small patches along the
   western coast) is through variance that is in common with the Southern
   Oscillation Index (SOI). In addition to forcing from the central/eastern
   tropical Pacific SST. there also appears a contribution from contrasting
   SST anomalies in the tropical Atlantic. This rainfall mode is usually a
   regional portion of a more large-scale mode encompassing at least the
   whole tropical zone (especially in DJFM, MAM and September-November.
   SON). Analysis of the relationship of this mode with GCM circulation
   features reveals that a rainfall deficit (respectively excedent) over
   the main rainbelt of the tropical America region is associated with
   strengthening (respectively weakening) of the sub-tropical westerly jet
   streams, a global warming (respectively cooling) of the tropical
   atmosphere. an anomalous divergence (respectively convergence) in the
   lower levels and an anomalous convergence (respectively divergence) in
   the upper levels over tropical America and in the region of the Atlantic
   Inter-tropical Convergence Zone (ITCZ). Such global features are not so
   apparent for the dominant mode of JJAS. even though the correlations
   with El Nino-Southern Oscillation (ENSO) indicators (as SOI or NINO3 SST
   index) are as high as for the other seasons.
   The bipolar N-S rainfall anomaly mode in tropical America is mostly
   related to anomalous N-S gradient of SST anomalies in the tropical
   Atlantic. The atmospheric circulation anomalies emphasize changes in 850
   hPa meridional winds in the tropical Atlantic. However, there is also
   interannual variance of this rainfall mode in both the model and
   observations that is unexplained by tropical Atlantic SSTs, but which is
   explained by central/eastern tropical Pacific SSTs and, potentially,
   SSTs from other tropical and extratropical areas. This is especially
   true in MAM.
   Some differences in the details of the model and observed teleconnection
   patterns are noted. Such differences can be used to statistically adjust
   the model simulations using the CCA or SVDA modes as basis patterns.
   Both statistical approaches have been applied and the results are
   consistent between the two, The increase of skill is stronger when
   temporal correlation (the pattern correlation) between the model and
   observed pattern is high (low) as for JJAS. The skill is moderate to
   high around the whole Amazon basin. but remains relatively low inside
   the Amazon basin, though reliability of the observations themselves may
   influence this result. Averaged over all the seasons, about 15-35\%
   (35-55\%) of the interannual grid-box (regional) seasonal rainfall
   variance is skilfully simulated from the observed SST forcing. Copyright
   (C) 2001 Royal Meteorological Society.}},
Publisher = {{WILEY}},
Address = {{111 RIVER ST, HOBOKEN 07030-5774, NJ USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Moron, V (Corresponding Author), CEREGE, UMR 6635, F-13545 Aix En Provence, France.
   CEREGE, UMR 6635, F-13545 Aix En Provence, France.
   Univ Aix Marseille 1, UFR Sci Geog \& Amenagement, Aix En Provence, France.
   Univ Oklahoma, CIMMS, Norman, OK 73019 USA.
   Columbia Univ, Lamont Doherty Earth Observ, IRI, New York, NY USA.
   CNR, ISAO, I-40126 Bologna, Italy.}},
DOI = {{10.1002/joc.690}},
ISSN = {{0899-8418}},
EISSN = {{1097-0088}},
Keywords = {{atmospheric General Circulation Model; Canonical Correlation Analysis;
   forecast skill; interannual variability; seasonal rainfall; sea-surface
   temperature forcing; Singular Value Decomposition Analysis; tropical
   America}},
Keywords-Plus = {{SEA-SURFACE TEMPERATURE; GENERAL-CIRCULATION MODEL; EXTREME CLIMATIC
   EVENTS; NORTHEAST BRAZIL; SOUTHERN-OSCILLATION; EL-NINO; INTERANNUAL
   VARIABILITY; ATMOSPHERIC RESPONSE; AIR TEMPERATURES; SYSTEMATIC-ERROR}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{moron@cerege.fr}},
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Number-of-Cited-References = {{78}},
Times-Cited = {{11}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{3}},
Journal-ISO = {{Int. J. Climatol.}},
Doc-Delivery-Number = {{488JP}},
Unique-ID = {{ISI:000171932300003}},
DA = {{2020-08-06}},
}

@article{ ISI:000172935100007,
Author = {Caskie, P and Davis, J and Wallace, M},
Title = {{Targeting disadvantage in agriculture}},
Journal = {{JOURNAL OF RURAL STUDIES}},
Year = {{2001}},
Volume = {{17}},
Number = {{4}},
Pages = {{471-479}},
Month = {{OCT}},
Abstract = {{The effectiveness of the main policy instrument targeting support at
   farmers in disadvantaged areas of the UK from 1976 to 2000 (the Hill
   Livestock Compensatory Allowance Scheme) is evaluated for Northern
   Ireland, using recursive linear programming models and input-output
   analysis. Capital. income and employment effects of the Scheme in its
   latter years are estimated and assessed against declared policy
   objectives. It is estimated that average farm cash incomes would have
   been between 17 and 31 per cent lower in the absence of HLCA payments,
   while farmer net worth would have fallen by approximately I per cent
   annually. In aggregate, some 1000 jobs were sustained by the Scheme and
   incomes and profits in the region were boosted by pound9 million each
   year. The main economic effect arising from the introduction of a
   successor area-based subsidy, will be a redistribution of payments from
   farms with relatively high stocking rates (predominantly larger units)
   to those operating more extensively (mostly smaller, part-time farms).
   (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 = {{Caskie, P (Corresponding Author), Queens Univ Belfast, Dept Agr \& Food Econ, Newforge Lane, Belfast BT9 5PX, Antrim, North Ireland.
   Queens Univ Belfast, Dept Agr \& Food Econ, Belfast BT9 5PX, Antrim, North Ireland.
   Univ Coll Dublin, Dept Agribusiness Extens \& Rural Dev, Dublin 4, Ireland.}},
DOI = {{10.1016/S0743-0167(01)00016-X}},
ISSN = {{0743-0167}},
Keywords = {{Less Favoured Areas; HLCA scheme; farm incomes; employment and capital
   base; environmental and cultural landscape; linear programming;
   input-output analysis}},
Research-Areas = {{Geography; Public Administration}},
Web-of-Science-Categories  = {{Geography; Regional \& Urban Planning}},
Author-Email = {{p.caskie@qub.ac.uk}},
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Number-of-Cited-References = {{24}},
Times-Cited = {{3}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{4}},
Journal-ISO = {{J. Rural Stud.}},
Doc-Delivery-Number = {{505UZ}},
Unique-ID = {{ISI:000172935100007}},
DA = {{2020-08-06}},
}

@article{ ISI:000171072800005,
Author = {de Garidel-Thoron, T and Beaufort, L and Linsley, BK and Dannenmann, S},
Title = {{Millennial-scale dynamics of the East Asian winter monsoon during the
   last 200,000 years}},
Journal = {{PALEOCEANOGRAPHY}},
Year = {{2001}},
Volume = {{16}},
Number = {{5}},
Pages = {{491-502}},
Month = {{OCT}},
Abstract = {{The primary productivity dynamics of the last 200,000 years in the Sulu
   Sea was reconstructed using the abundance of the coccolithophore
   Florisphaera profunda in the IMAGES MD97-2141 core. We find that primary
   productivity was enhanced during glacial periods, which we suggest is
   due to a stronger East Asian winter monsoon. During the last 80 kyr,
   eight significant increases in primary productivity (PP) in the Sulu Sea
   are similar to East Asian winter monsoon changes recorded in Chinese
   loess. The PP maxima are not linked with Heinrich events (HE) in the
   North Atlantic, although four PP peaks are synchronous with HE. The PP
   oscillations have frequencies near those of the Dansgaard-Oeschger
   cycles in Northern Hemisphere ice records and indicate a teleconnection
   of the East Asian winter monsoon with Greenland climate. In this Sulu
   Sea record the East Asian winter monsoon oscillates with periodicities
   of similar to6, 4.2-3.4, 2.3, and 1.5 kyr. In particular, the 1.5 kyr
   cycle exhibits a strong and pervasive signal from stage 6 to the
   Holocene without any ice volume modulation. This stationarity suggests
   that the 1.5 kyr cycle is not driven by some high-latitude forcing.}},
Publisher = {{AMER GEOPHYSICAL UNION}},
Address = {{2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{de Garidel-Thoron, T (Corresponding Author), Ctr Europeen Rech \& Enseignement Geosci, Europole Mediterraneen Arbois, BP 80, F-13545 Aix En Provence 4, France.
   Ctr Europeen Rech \& Enseignement Geosci, Europole Mediterraneen Arbois, F-13545 Aix En Provence 4, France.
   SUNY Albany, Dept Earth \& Atmospher Sci, Albany, NY 12222 USA.}},
DOI = {{10.1029/2000PA000557}},
ISSN = {{0883-8305}},
EISSN = {{1944-9186}},
Keywords-Plus = {{WESTERN EQUATORIAL PACIFIC; SEA-SURFACE TEMPERATURE; YOUNGER DRYAS
   EVENT; SOUTH CHINA SEA; NORTH-ATLANTIC; SULU SEA; PALEOCLIMATIC
   VARIABILITY; CLIMATE OSCILLATIONS; OCEAN; HOLOCENE}},
Research-Areas = {{Geology; Oceanography; Paleontology}},
Web-of-Science-Categories  = {{Geosciences, Multidisciplinary; Oceanography; Paleontology}},
Author-Email = {{garidel@cerege.fr}},
ResearcherID-Numbers = {{de Garidel-Thoron, Thibault/B-1204-2008
   }},
ORCID-Numbers = {{de Garidel-Thoron, Thibault/0000-0001-8983-9571
   Linsley, Braddock/0000-0003-2085-0662
   Beaufort, Luc/0000-0001-6055-9373}},
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Number-of-Cited-References = {{64}},
Times-Cited = {{73}},
Usage-Count-Last-180-days = {{2}},
Usage-Count-Since-2013 = {{31}},
Journal-ISO = {{Paleoceanography}},
Doc-Delivery-Number = {{473WW}},
Unique-ID = {{ISI:000171072800005}},
DA = {{2020-08-06}},
}

@article{ ISI:000171044200003,
Author = {Su, H and Neelin, JD and Chou, C},
Title = {{Tropical teleconnection and local response to SST anomalies during the
   1997-1998 El Nino}},
Journal = {{JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES}},
Year = {{2001}},
Volume = {{106}},
Number = {{D17}},
Pages = {{20025-20043}},
Month = {{SEP 16}},
Abstract = {{The quasi-equilibrium tropical circulation model (QTCM) is used to
   examine the response to various sea surface temperature (SST) anomalies
   in the tropical oceans during the 1997-1998 El Nino. Both local and
   remote responses are noted. The negative precipitation anomalies to the
   north and south of the El Nino - Southern Oscillation (ENSO) enhanced
   precipitation region are largely a response to the warm SST anomalies in
   the central and eastern Pacific. However, in the western Pacific and
   maritime continent, reduction of rainfall is mainly caused by local cold
   SST anomalies. In the winter of the 1997-1998 El Nino, strong warm SST
   anomalies in the Indian Ocean contributed to the local enhanced
   rainfall. They affect precipitation anomalies in central, eastern, and
   southern Africa. The drought in northern South America is clearly a
   remote response to ENSO warm SST anomalies in the Pacific, while the SST
   anomalies in the Atlantic also impact the drought. The tropical Pacific
   cold SST anomalies surrounding the ENSO warm anomalies appear not to be
   caused by surface flux changes associated with atmospheric
   teleconnection (in simulations with specified SST in the ENSO warm
   region and a mixed-layer ocean model elsewhere). Atmospheric circulation
   tends to spread the warm anomalies, but ocean dynamics appears also to
   be important for both cold and warm SST anomalies outside the equatorial
   upwelling region. In both the regional specified SST experiments and
   mixed-layer experiments, relative subsidence tends to occur within
   convective zones, and it is generally localized. On the other hand,
   tropospheric temperature and wind anomalies spread much farther. The
   typical spatial scale of the remote response in temperature and wind
   fields tends to be larger than the dominant scale of the precipitation
   response. The remote response in precipitation anomalies does not appear
   to be related to temperature and wind anomalies in a simple manner.}},
Publisher = {{AMER GEOPHYSICAL UNION}},
Address = {{2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Su, H (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.
   Univ Calif Los Angeles, Inst Geophys \& Planetary Phys, Los Angeles, CA 90024 USA.}},
DOI = {{10.1029/2000JD000124}},
ISSN = {{2169-897X}},
EISSN = {{2169-8996}},
Keywords-Plus = {{SEA-SURFACE TEMPERATURE; SOUTHERN-OSCILLATION; INDIAN-OCEAN; CIRCULATION
   MODEL; ATMOSPHERIC RESPONSE; CLIMATE VARIABILITY; RAINFALL ANOMALIES;
   SAHEL RAINFALL; PACIFIC-OCEAN; ENSO}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{hui@atmos.ucla.edu
   neelin@atmos.ucla.edu
   chia@atmos.ucla.edu}},
ResearcherID-Numbers = {{Chou, Chia/D-1479-2012
   Neelin, J. David/H-4337-2011}},
ORCID-Numbers = {{Chou, Chia/0000-0001-9192-4724
   }},
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Number-of-Cited-References = {{47}},
Times-Cited = {{64}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{14}},
Journal-ISO = {{J. Geophys. Res.-Atmos.}},
Doc-Delivery-Number = {{473KZ}},
Unique-ID = {{ISI:000171044200003}},
DA = {{2020-08-06}},
}

@article{ ISI:000171382500006,
Author = {Zhou, WJ and Head, MJ and An, ZS and De Deckker, P and Liu, ZY and Liu,
   XD and Lu, XF and Donahue, D and Jull, AJT and Beck, JW},
Title = {{Terrestrial evidence for a spatial structure of tropical-polar
   interconnections during the Younger Dryas episode}},
Journal = {{EARTH AND PLANETARY SCIENCE LETTERS}},
Year = {{2001}},
Volume = {{191}},
Number = {{3-4}},
Pages = {{231-239}},
Month = {{SEP 15}},
Abstract = {{The Younger Dryas chronozone, recognised in northern high-latitude areas
   as a cold event between 11 000 and 10 000 C-14 yr BP (12 900-11 600 cal.
   yr BP), seems to manifest itself globally in different ways. Here, we
   examine well-dated stratigraphic sequences together with high-resolution
   proxy data plots from sites across our study area, the arid-semi-arid
   transition zone in northern China. This climatically sensitive area of
   China records a cold, dry Younger Dryas climate which was punctuated by
   a brief period of summer monsoon precipitation. We have since found that
   similar climatic sequences have been reported from the Sahel and the
   equatorial region of Africa. Based on evidence from these sites,
   together with other published data, we postulate that precipitation
   during the Younger Dryas chronozone was indicative of a low-latitude
   driving force superimposed on the high-latitude cold background. This
   rain belt rearrangement was most probably caused by an interaction
   between cold air advection and summer moisture transport across the
   tropical Pacific Ocean. Examination of high-resolution proxies suggests
   short-term climate fluctuations indicative of a global teleconnection
   involving moist air transportation patterns from the tropics to higher
   latitudes, varying with ENSO and other tropical factors. (C) 2001
   Elsevier Science B.V. All rights reserved.}},
Publisher = {{ELSEVIER SCIENCE BV}},
Address = {{PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Zhou, WJ (Corresponding Author), Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess \& Quaternary Geol, POB 17, Xian 710054, Peoples R China.
   Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess \& Quaternary Geol, Xian 710054, Peoples R China.
   Australian Natl Univ, Fac Sci, Dept Geol, Canberra, ACT 0200, Australia.
   Univ Wisconsin, Dept Atmospher \& Ocean Sci, Madison, WI 53706 USA.
   Univ Arizona, NSF Arizona AMS Facil, Tucson, AZ 85721 USA.
   Univ Wollongong, Sch Geosci, Wollongong, NSW 2522, Australia.}},
DOI = {{10.1016/S0012-821X(01)00416-2}},
ISSN = {{0012-821X}},
Keywords = {{Younger Dryas; paleoclimatology; global change; paleo-oceanography;
   general circulation models; Southern Oscillation; El Nino; North
   Atlantic oscillation; desert-loess transition zone}},
Keywords-Plus = {{LAST DEGLACIATION; MONSOON CLIMATE; LATE QUATERNARY; NORTH-ATLANTIC;
   EAST-AFRICA; KYR BP; RECORD; EVENT; TEMPERATURE; OCEAN}},
Research-Areas = {{Geochemistry \& Geophysics}},
Web-of-Science-Categories  = {{Geochemistry \& Geophysics}},

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