text:
, GL (Corresponding Author), Natl Climate Res Ctr CMA, Lab Climate Studies, Zhongguancun South St 46, Beijing 100081, Peoples R China.
   Gong, Zhiqiang; Feng, Guolin, Natl Climate Res Ctr CMA, Lab Climate Studies, Zhongguancun South St 46, Beijing 100081, Peoples R China.
   Dogar, Muhammad Mubashar, King Abdullah Univ Sci \& Technol, Earth Sci \& Engn Dept, Thuwal, Saudi Arabia.
   Dogar, Muhammad Mubashar, Minist Climate Change, Global Change Impact Studies Ctr, Islamabad, Pakistan.
   Qiao, Shaobo; Hu, Po; Feng, Guolin, Lanzhou Univ, Coll Atmospher Sci, Lanzhou, Gansu, Peoples R China.}},
DOI = {{10.1002/joc.5327}},
ISSN = {{0899-8418}},
EISSN = {{1097-0088}},
Keywords = {{leading modes; assessment; prediction; dynamic-statistic combined
   correction}},
Keywords-Plus = {{TELECONNECTION PATTERN; DECADAL CHANGE; EAST-ASIA; PREDICTION; MONSOON;
   RAINFALL; VARIABILITY; CHINA; DYNAMICS; SYSTEM}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{fenggl@cma.gov.cn}},
ResearcherID-Numbers = {{Dogar, Muhammad/AAK-3964-2020}},
Funding-Acknowledgement = {{Special Scientific Research Project for Public Interest
   {[}GYHY201306021]; National Natural Science Foundation of ChinaNational
   Natural Science Foundation of China {[}41475064, 41575082]}},
Funding-Text = {{The authors wish to thank three anonymous reviewers' meaningful comments
   that led to a much-improved manuscript. This work is supported by the
   National Natural Science Foundation of China (Grant Nos. 41575082 and
   41475064), the Special Scientific Research Project for Public Interest
   (Grant No. GYHY201306021).}},
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Number-of-Cited-References = {{47}},
Times-Cited = {{6}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{10}},
Journal-ISO = {{Int. J. Climatol.}},
Doc-Delivery-Number = {{GB2KG}},
Unique-ID = {{ISI:000428880600005}},
OA = {{Green Published}},
DA = {{2020-08-06}},
}

@article{ ISI:000428880600034,
Author = {Piao, Jinling and Chen, Wen and Chen, Shangfeng and Wei, Ke},
Title = {{Intensified impact of North Atlantic Oscillation in May on subsequent
   July Asian inland plateau precipitation since the late 1970s}},
Journal = {{INTERNATIONAL JOURNAL OF CLIMATOLOGY}},
Year = {{2018}},
Volume = {{38}},
Number = {{5}},
Pages = {{2605-2612}},
Month = {{APR}},
Abstract = {{The relationship between the North Atlantic Oscillation (NAO) in May and
   precipitation in the Asian inland plateau (AIP) in following July has
   experienced a significant enhancement since the late 1970s. This study
   investigates the factors for this inter-decadal change of the NAO-AIP
   precipitation connection. Before the late 1970s, geopotential height
   anomalies related to the May NAO exhibited a dipole pattern confined to
   the North Atlantic from May to June and decayed in July. As a result,
   the impact of the May NAO on the AIP precipitation in July is weak. In
   contrast, after the late 1970s, geopotential height anomalies associated
   with the May NAO persisted into July. The analysis in this study finds
   that the May NAO influences July AIP precipitation via modulating the
   Polar-Eurasia teleconnection (POL). After (before) the late 1970s, the
   connection between the May NAO and the POL was strong (weak), explaining
   the inter-decadal change in the May NAO-July AIP precipitation
   relationship. Further analysis suggests that the strengthening of the
   relationship between the May NAO pattern and the July POL after the late
   1970s may be attributed to the inter-decadal contraction of the Northern
   Hemisphere circumpolar vortex.}},
Publisher = {{WILEY}},
Address = {{111 RIVER ST, HOBOKEN 07030-5774, NJ USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Chen, W (Corresponding Author), Chinese Acad Sci, Inst Atmospher Phys, Ctr Monsoon Syst Res, Beijing 100190, Peoples R China.
   Piao, Jinling; Chen, Wen; Chen, Shangfeng; Wei, Ke, Chinese Acad Sci, Inst Atmospher Phys, Ctr Monsoon Syst Res, Beijing 100190, Peoples R China.
   Piao, Jinling; Chen, Wen, Univ Chinese Acad Sci, Sch Earth Sci, Beijing, Peoples R China.}},
DOI = {{10.1002/joc.5332}},
ISSN = {{0899-8418}},
EISSN = {{1097-0088}},
Keywords = {{Asian inland plateau; July precipitation; North Atlantic Oscillation;
   Polar-Eurasia pattern}},
Keywords-Plus = {{HEMISPHERE CIRCUMPOLAR VORTEX; SEA-SURFACE TEMPERATURE; ATMOSPHERIC
   CIRCULATION; SUMMER MONSOON; ARCTIC OSCILLATION; TIBETAN PLATEAU;
   INNER-MONGOLIA; CLIMATE; RAINFALL; WINTER}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{cw@post.iap.ac.cn}},
ResearcherID-Numbers = {{chen, Shangfeng/AAP-2223-2020
   chen, shangfeng/AAO-9288-2020
   Chen, Wen/G-6058-2011}},
ORCID-Numbers = {{chen, shangfeng/0000-0003-4347-8592
   Chen, Wen/0000-0001-9327-9079}},
Funding-Acknowledgement = {{Jiangsu Collaborative Innovation Center for Climate Change; National Key
   Research and Development Program {[}2016YFA0600604]; National Natural
   Science Foundation of ChinaNational Natural Science Foundation of China
   {[}41605050, 41230527]}},
Funding-Text = {{We thank two anonymous reviewers for their constructive suggestions and
   comments, which helped to improve the article. This study was supported
   jointly by the National Key Research and Development Program (grant no.
   2016YFA0600604), the National Natural Science Foundation of China (grant
   nos. 41230527 and 41605050), and the Jiangsu Collaborative Innovation
   Center for Climate Change. Authors declare that they have no conflict of
   interest.}},
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Number-of-Cited-References = {{51}},
Times-Cited = {{4}},
Usage-Count-Last-180-days = {{8}},
Usage-Count-Since-2013 = {{20}},
Journal-ISO = {{Int. J. Climatol.}},
Doc-Delivery-Number = {{GB2KG}},
Unique-ID = {{ISI:000428880600034}},
DA = {{2020-08-06}},
}

@article{ ISI:000428880600036,
Author = {Yu, Tianlei and Cheng, Jun and Lin, Pengfei and Yu, Yongqiang and Guo,
   Pinwen},
Title = {{Responses and mechanisms of East Asian winter and summer monsoons to
   weakened Atlantic meridional overturning circulation using the FGOALS-g2
   model}},
Journal = {{INTERNATIONAL JOURNAL OF CLIMATOLOGY}},
Year = {{2018}},
Volume = {{38}},
Number = {{5}},
Pages = {{2618-2626}},
Month = {{APR}},
Abstract = {{This study investigates the responses and mechanisms of East Asian
   winter monsoon (EAWM) and East Asian summer monsoon (EASM) to weakened
   Atlantic meridional overturning circulation (AMOC) through three
   perturbation experiments with different intensities of freshwater hosing
   in the North Atlantic, using the Flexible Global Ocean -Atmosphere -
   Land System Model, Grid-point Version 2. These experiments show that a
   subtle weakening of AMOC does not significantly influence either the
   EAWM or the EASM. When AMOC weakens more substantially, northerly wind
   anomalies emerge in East Asia throughout the year, strengthening the
   EAWM and weakening the EASM. The northerly wind anomalies result from an
   anomalous westward sea level pressure (SLP) gradient, namely positive
   SLP anomalies across Eurasia and negative anomalies in the western North
   Pacific (WNP). In winter, negative WNP SLP anomalies are found in
   mid-high latitudes. They are caused by anomalous stationary wave
   activity, which is associated with the Aleutian Iceland seesaw
   teleconnection. In summer, negative WNP SLP anomalies are present in the
   subtropics, and are linked with an anomalous cyclonic circulation over
   the north of the Philippian Sea. This cyclonic circulation anomaly is
   induced by the anomalous warm water in the subsurface of the South China
   Sea and Philippian Sea through the Gill mechanism.}},
Publisher = {{WILEY}},
Address = {{111 RIVER ST, HOBOKEN 07030-5774, NJ USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Cheng, J (Corresponding Author), Nanjing Univ Informat Sci \& Technol, Collaborat Innovat Ctr Forecast \& Evaluat Meteoro, Key Lab Meteorol Disaster, Minist Educ, Ningliu Rd 219, Nanjing 210044, Jiangsu, Peoples R China.
   Yu, Tianlei; Cheng, Jun; Guo, Pinwen, Nanjing Univ Informat Sci \& Technol, Collaborat Innovat Ctr Forecast \& Evaluat Meteoro, Key Lab Meteorol Disaster, Minist Educ,Climate Dynam Res Ctr, Nanjing, Jiangsu, Peoples R China.
   Lin, Pengfei; Yu, Yongqiang, Univ Chinese Acad Sci, Coll Earth Sci, Beijing, Peoples R China.
   Lin, Pengfei; Yu, Yongqiang, Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci \& Geop, Beijing, Peoples R China.}},
DOI = {{10.1002/joc.5373}},
ISSN = {{0899-8418}},
EISSN = {{1097-0088}},
Keywords = {{Atlantic meridional overturning circulation; freshwater hosing
   experiment; East Asian monsoon; FGOALS-g2}},
Keywords-Plus = {{COUPLED CLIMATE MODELS; THERMOHALINE CIRCULATION; TROPICAL ATLANTIC;
   VARIABILITY; PACIFIC; ATMOSPHERE; AMERICAN; COLLAPSE; IMPACTS}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{chengjun@nuist.edu.cn}},
ResearcherID-Numbers = {{Lin, Pengfei/AAJ-5379-2020
   Yu, Yongqiang/K-7808-2012
   }},
ORCID-Numbers = {{Lin, Pengfei/0000-0003-2361-0066
   Yu, Yongqiang/0000-0001-8596-3583
   Cheng, Jun/0000-0003-0168-1410
   Tianlei, Yu/0000-0002-6962-2575}},
Funding-Acknowledgement = {{Global Change Program of National Key Research and Development Program
   of China {[}2016YFA0600504, 2015CB953902]; National Natural Science
   Foundation of ChinaNational Natural Science Foundation of China
   {[}41630527, 41376019, 41206024]; Priority Academic Program Development
   of Jiangsu Higher Education Institutions (PAPD); Research Innovation
   Program for college graduates of Jiangsu Province {[}KYLX\_0826]}},
Funding-Text = {{We sincerely thank the two anonymous reviewers for their helpful
   comments and suggestions on the manuscript. Also, we acknowledge
   Professor Hiajun Yang for providing their freshwater forcing
   experimental data. This work is supported by the Global Change Program
   of National Key Research and Development Program of China (grants
   2016YFA0600504 and 2015CB953902), the National Natural Science
   Foundation of China (grants 41630527, 41376019 and 41206024) and Qing
   Lan project and project funded by the Priority Academic Program
   Development of Jiangsu Higher Education Institutions (PAPD). Tianlei Yu
   was also supported by the Research Innovation Program for college
   graduates of Jiangsu Province (KYLX\_0826). We declare no conflict of
   interests.}},
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Number-of-Cited-References = {{42}},
Times-Cited = {{2}},
Usage-Count-Last-180-days = {{2}},
Usage-Count-Since-2013 = {{16}},
Journal-ISO = {{Int. J. Climatol.}},
Doc-Delivery-Number = {{GB2KG}},
Unique-ID = {{ISI:000428880600036}},
DA = {{2020-08-06}},
}

@article{ ISI:000429716700009,
Author = {Beylot, Antoine and Boitier, Baptiste and Lancesseur, Nicolas and
   Villeneuve, Jacques},
Title = {{The Waste Footprint of French Households in 2020 A Comparison of
   Scenarios of Consumption Growth Using Input-Output Analysis}},
Journal = {{JOURNAL OF INDUSTRIAL ECOLOGY}},
Year = {{2018}},
Volume = {{22}},
Number = {{2}},
Pages = {{356-368}},
Month = {{APR}},
Abstract = {{This study aims at quantifying and analyzing the waste footprint of
   French household consumption in 2020 with respect to different scenarios
   of economic growth. Three models are jointly used: (1) a multiregional
   unilateral input-output model extended to waste, to quantify waste
   generation from economic activities induced by household consumption;
   (2) a coefficient-based model dedicated to quantifying post-consumer
   waste as a function of household consumption; and (3) the New
   Econometric Model of Evaluation by Sectorial Interdependency and Supply
   (NEMESIS), a macroeconometric model used to elaborate different
   scenarios of growth in household consumption in the period 2008-2020.
   Three scenarios consider changes primarily in terms of household
   consumption volume, while one scenario additionally considers changes in
   the composition of consumption according to the past-30-year trend.
   First, this study suggests that if the trend in changes of composition
   is maintained, it will lead, by 2020, to a ``relative{''} decoupling
   between French household consumption and waste footprint with respect to
   dry recyclables, mixed wastes, and organic wastes and to an
   ``absolute{''} decoupling with respect to mineral wastes. Second, this
   study provides a mapping of the changes in French household waste
   footprints from 2008 to 2020 as a function of scenarios, with
   indications of where these changes would actually occur in the economy
   (waste from economic activities or postconsumer waste) and
   geographically (in France or abroad). In particular, for most of the
   scenarios considered, changes in French household consumption from 2008
   to 2020 primarily induce changes in organic and mineral waste generation
   abroad rather than in France.}},
Publisher = {{WILEY}},
Address = {{111 RIVER ST, HOBOKEN 07030-5774, NJ USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Beylot, A (Corresponding Author), Bur Rech Geol \& Minieres, BP 6009,3 Av C Guillemin, F-45060 Orleans, France.
   Beylot, Antoine; Villeneuve, Jacques, Bur Rech Geol \& Minieres, BP 6009,3 Av C Guillemin, F-45060 Orleans, France.
   Boitier, Baptiste; Lancesseur, Nicolas, SEURECO, Paris, France.
   Lancesseur, Nicolas, Univ Paris Est Creteil, Paris, France.}},
DOI = {{10.1111/jiec.12566}},
ISSN = {{1088-1980}},
EISSN = {{1530-9290}},
Keywords = {{decoupling; economic growth; input-output analysis (IOA); sustainable
   consumption; waste footprint; waste generation}},
Keywords-Plus = {{POLICY}},
Research-Areas = {{Science \& Technology - Other Topics; Engineering; Environmental
   Sciences \& Ecology}},
Web-of-Science-Categories  = {{Green \& Sustainable Science \& Technology; Engineering, Environmental;
   Environmental Sciences}},
Author-Email = {{a.beylot@brgm.fr}},
Funding-Acknowledgement = {{French Environment and Energy Management Agency (ADEME)}},
Funding-Text = {{This study was partly funded by the French Environment and Energy
   Management Agency (ADEME) in the framework of the Reactivity project.}},
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Number-of-Cited-References = {{39}},
Times-Cited = {{5}},
Usage-Count-Last-180-days = {{3}},
Usage-Count-Since-2013 = {{14}},
Journal-ISO = {{J. Ind. Ecol.}},
Doc-Delivery-Number = {{GC3XJ}},
Unique-ID = {{ISI:000429716700009}},
DA = {{2020-08-06}},
}

@article{ ISI:000430662300001,
Author = {Li, Xinyu and Gollan, Gereon and Greatbatch, Richard J. and Lu, Riyu},
Title = {{Intraseasonal variation of the East Asian summer monsoon associated with
   the Madden-Julian Oscillation}},
Journal = {{ATMOSPHERIC SCIENCE LETTERS}},
Year = {{2018}},
Volume = {{19}},
Number = {{4}},
Month = {{APR}},
Abstract = {{We investigate the daily variability of the East Asian summer monsoon
   (EASM) by projecting daily wind anomaly data onto the two major modes of
   an interannual multivariate Empirical Orthogonal Functions analysis.
   Mode 1, closely resembling the Pacific-Japan (PJ) pattern and referred
   to as PJ-mode, transits from positive to negative phase around
   mid-summer consistent with the Meiyu rains predominantly being an early
   summer phenomenon. Mode 2, which is influenced by the Indian summer
   monsoon (ISM) and referred to as ISM-mode, peaks in late July and early
   August and is associated with rainfall farther north over China. We then
   analyze the relation between the intraseasonal variation of the EASM and
   the Madden-Julian Oscillation (MJO) by analyzing circulation anomalies
   following MJO events. In the lower troposphere, the circulation
   anomalies associated with the MJO most strongly project on the PJ-mode.
   MJO phases 1-4 (5-8) favor the positive (negative) phase of the PJ-mode
   by favoring the anticyclonic (cyclonic) anomalies over the subtropical
   western North Pacific. In the upper troposphere, the circulation
   anomalies associated with the MJO project mainly on the ISM-mode.}},
Publisher = {{WILEY}},
Address = {{111 RIVER ST, HOBOKEN 07030-5774, NJ USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Gollan, G (Corresponding Author), GEOMAR Helmholtz Ctr Ocean Res Kiel, Dusternbrooker Weg 20, D-24105 Kiel, Germany.
   Li, Xinyu; Lu, Riyu, Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci \& Geop, Beijing, Peoples R China.
   Li, Xinyu; Lu, Riyu, Univ Chinese Acad Sci, Beijing, Peoples R China.
   Li, Xinyu; Gollan, Gereon; Greatbatch, Richard J., GEOMAR Helmholtz Ctr Ocean Res Kiel, RD Ocean Circulat \& Climate Dynam, Kiel, Germany.
   Greatbatch, Richard J., Univ Kiel, Fac Math \& Nat Sci, Kiel, Germany.}},
DOI = {{10.1002/asl.794}},
Article-Number = {{UNSP e794}},
ISSN = {{1530-261X}},
Keywords = {{East Asian summer monsoon; intraseasonal variation; MJO}},
Keywords-Plus = {{NORTHERN-HEMISPHERE SUMMER; CIRCUMGLOBAL TELECONNECTION; ZONAL WIND;
   VARIABILITY; PACIFIC; CIRCULATION; IMPACT; MODES; MJO}},
Research-Areas = {{Geochemistry \& Geophysics; Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Geochemistry \& Geophysics; Meteorology \& Atmospheric Sciences}},
Author-Email = {{ggollan@geomar.de}},
ResearcherID-Numbers = {{Li, Lambert LL/F-7146-2015}},
Funding-Acknowledgement = {{Bundesministerium fur Bildung und ForschungFederal Ministry of Education
   \& Research (BMBF) {[}01LP1517D]; German Academic Exchange
   ServiceDeutscher Akademischer Austausch Dienst (DAAD) {[}01LP1517D]}},
Funding-Text = {{Bundesministerium fur Bildung und Forschung, Grant/Award number:
   01LP1517D; German Academic Exchange Service, Grant/Award number:
   01LP1517D}},
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Number-of-Cited-References = {{24}},
Times-Cited = {{5}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{12}},
Journal-ISO = {{Atmos. Sci. Lett.}},
Doc-Delivery-Number = {{GD7AZ}},
Unique-ID = {{ISI:000430662300001}},
OA = {{DOAJ Gold, Green Accepted}},
DA = {{2020-08-06}},
}

@article{ ISI:000429456500013,
Author = {Revelard, Adele and Frankignoul, Claude and Kwon, Young-Oh},
Title = {{A Multivariate Estimate of the Cold Season Atmospheric Response to North
   Pacific SST Variability}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2018}},
Volume = {{31}},
Number = {{7}},
Pages = {{2771-2796}},
Month = {{APR}},
Abstract = {{The Generalized Equilibrium Feedback Analysis (GEFA) is used to
   distinguish the influence of the Oyashio Extension (OE) and the Kuroshio
   Extension (KE) variability on the atmosphere from 1979 to 2014 from that
   of the main SST variability modes, using seasonal mean anomalies. Remote
   SST anomalies are associated with each single oceanic regressor, but the
   multivariate approach efficiently confines their SST footprints. In
   autumn {[}October-December (OND)], the OE meridional shifts are followed
   by a North Pacific Oscillation (NPO)-like signal. The OE influence is
   not investigated in winter {[}December-February (DJF)] because of
   multicollinearity, but a robust response with a strong signal over the
   Bering Sea is found in late winter/early spring {[}February-April
   (FMA)], a northeastward strengthening of the Aleutian low following a
   northward OE shift. A robust response to the KE variability is found in
   autumn, but not in winter and late winter when the KE SST footprint
   becomes increasingly small and noisy as regressors are added in GEFA. In
   autumn, a positivePDOis followed by a northward strengthening of the
   Aleutian low and a southward shift of the storm track in the central
   Pacific, reflecting the surface heat flux footprint in the central
   Pacific. In winter, the PDO shifts the maximum baroclinicity and storm
   track southward, the response strongly tilts westward with height in the
   North Pacific, and there is a negative NAO-like teleconnection. In late
   winter, the North Pacific NPO-like response to the PDO interferes
   negatively with the response to the OE and is only detected when the OE
   is represented in GEFA. A different PDO influence on the atmospheric
   circulation is found from 1958 to 1977.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Frankignoul, C (Corresponding Author), Sorbonne Univ, LOCEAN IPSL, Paris, France.
   Revelard, Adele; Frankignoul, Claude, Sorbonne Univ, LOCEAN IPSL, Paris, France.
   Kwon, Young-Oh, Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA.}},
DOI = {{10.1175/JCLI-D-17-0061.1}},
ISSN = {{0894-8755}},
EISSN = {{1520-0442}},
Keywords-Plus = {{SURFACE TEMPERATURE ANOMALIES; ERA-INTERIM REANALYSIS; KUROSHIO
   EXTENSION; DECADAL VARIABILITY; STORM TRACKS; GULF-STREAM; GLOBAL
   OCEANS; COUPLED MODEL; INDIAN-OCEAN; ATLANTIC SST}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{cf@locean-ipsl.upmc.fr}},
ResearcherID-Numbers = {{Kwon, Young-Oh/C-2190-2008
   }},
ORCID-Numbers = {{Kwon, Young-Oh/0000-0002-1241-2817
   Revelard, Adele/0000-0002-0845-1434}},
Funding-Acknowledgement = {{European UnionEuropean Union (EU) {[}308299]; NSFNational Science
   Foundation (NSF) {[}AGS CLD 1035423, OCE PO 1242989]}},
Funding-Text = {{This research has received funding from the European Union 7th Framework
   Program (FP7 2007-2013) under Grant Agreement 308299 (NACLIM) and from
   NSF Grants AGS CLD 1035423 and OCE PO 1242989. We thank the reviewers
   for their thoughtful and constructive comments.}},
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Number-of-Cited-References = {{81}},
Times-Cited = {{3}},
Usage-Count-Last-180-days = {{4}},
Usage-Count-Since-2013 = {{21}},
Journal-ISO = {{J. Clim.}},
Doc-Delivery-Number = {{GC0GW}},
Unique-ID = {{ISI:000429456500013}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000429734200010,
Author = {Wu, Feng and Zhang, Qian and Gao, Xing},
Title = {{Does water-saving technology reduce water use in economic systems? A
   rebound effect in Zhangye city in the Heihe River Basin, China}},
Journal = {{WATER POLICY}},
Year = {{2018}},
Volume = {{20}},
Number = {{2}},
Pages = {{355-368}},
Month = {{APR}},
Abstract = {{As water use is closely associated with economic activities, a growing
   population, agricultural development, and reallocation of water
   resources, the Heihe River Basin highlights common issues of water
   productivity and ground-water overexploitation. We conducted a
   quasi-dynamic input-output analysis to investigate the changes to water
   use among different sectors of Zhangye city from 2002 to 2012, and
   clarified the driving mechanism of these changes. Our results indicated
   that the direct agricultural water use coefficient (calculated with an
   input-output table and other water use data) was the largest among the
   coefficients from all the sectors; notably, the fishery sector still
   consumed about 1 m(3) of water per unit output in 2012. We found that
   the water-saving technologies clearly contributed to the decrease of
   agricultural water from 2002 to 2007, but induced a rebound in total
   water use from 2007 to 2012. This study provides insights into the
   challenges of water resource management in the Heihe River Basin and
   sheds light on potential water-saving strategies for the future. This
   study may also enhance the policy relevance of land use governance and
   industrial transformation. A comprehensive exploration of the
   water-ecosystem economy is critical to integrated water resource
   management.}},
Publisher = {{IWA PUBLISHING}},
Address = {{ALLIANCE HOUSE, 12 CAXTON ST, LONDON SW1H0QS, ENGLAND}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Wu, F (Corresponding Author), Chinese Acad Sci, Inst Geog Sci \& Nat Resources Res, Beijing 100101, Peoples R China.
   Wu, F (Corresponding Author), Chinese Acad Sci, Ctr Chinese Agr Policy, Beijing 100101, Peoples R China.
   Wu, Feng; Zhang, Qian; Gao, Xing, Chinese Acad Sci, Inst Geog Sci \& Nat Resources Res, Beijing 100101, Peoples R China.
   Wu, Feng; Zhang, Qian, Chinese Acad Sci, Ctr Chinese Agr Policy, Beijing 100101, Peoples R China.}},
DOI = {{10.2166/wp.2017.003}},
ISSN = {{1366-7017}},
Keywords = {{Input-output model; Integrated water resource management; Rebound
   effect; Water-saving technology}},
Keywords-Plus = {{INPUT-OUTPUT-ANALYSIS; CONSUMPTION; RESOURCES; TRADE; TABLE}},
Research-Areas = {{Water Resources}},
Web-of-Science-Categories  = {{Water Resources}},
Author-Email = {{wufeng@igsnrr.ac.cn}},
Funding-Acknowledgement = {{National Natural Science Foundation (NSFC) of ChinaNational Natural
   Science Foundation of China {[}91325302, 91425303, 41671526]; Director
   Innovation Fund - Institute of Geographical Sciences and Natural
   Resources Research}},
Funding-Text = {{This research was financially supported by projects of the National
   Natural Science Foundation (NSFC) of China (91325302, 91425303, and
   41671526) and Director Innovation Fund sponsored by the Institute of
   Geographical Sciences and Natural Resources Research.}},
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Number-of-Cited-References = {{28}},
Times-Cited = {{5}},
Usage-Count-Last-180-days = {{2}},
Usage-Count-Since-2013 = {{35}},
Journal-ISO = {{Water Policy}},
Doc-Delivery-Number = {{GC4DQ}},
Unique-ID = {{ISI:000429734200010}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000428974500006,
Author = {Moreau, Vincent and Vuille, Francois},
Title = {{Decoupling energy use and economic growth: Counter evidence from
   structural effects and embodied energy in trade}},
Journal = {{APPLIED ENERGY}},
Year = {{2018}},
Volume = {{215}},
Pages = {{54-62}},
Month = {{APR 1}},
Abstract = {{Decoupling economic growth from energy consumption is a wide spread
   attempt to decarbonize economic activities and increase energy security.
   Almost all members of the European Union have decoupled the two since
   2005 as measured by a steady decline in energy intensity, the ratio of
   final energy consumption and gross domestic product. Economic growth,
   energy efficiency and structural changes have all contributed to changes
   in energy intensity of economic activities at the national level. In
   this article, the authors analyze to what extent decoupling can be
   attributed to each of these three factors and in particular structural
   effects, namely deindustrialization and tertiarization, which shifts
   energy consumption abroad and re-imports it as embodied energy in
   products.
   We quantify the effects of structural changes, economic growth and
   energy efficiency measures as well as embodied energy in trade at the
   level of economic activities. The methodological approach combines
   decomposition and input-output analysis to address boundary cases where
   monetary trade surpluses meet energy trade deficits. Switzerland
   provides a case in point with the added hurdle of low data availability
   per economic activity over time.
   The results show that the share of embodied energy in imports has
   reached 81\% of final energy consumption in economic activities. A
   comparison of energy intensities with and without embodied energy in
   trade shows that decoupling is more virtual than actual. Shifting energy
   intensive activities abroad improves domestic performance but worsens
   both overall energy use and security by relying on more indirect energy
   consumption. Energy indicators should therefore be adjusted to avoid
   potentially conflicting policy objectives between energy intensity and
   security as well as trade.}},
Publisher = {{ELSEVIER SCI LTD}},
Address = {{THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Vuille, F (Corresponding Author), Ecole Polytech Fed Lausanne, Energy Ctr, BAC 104,Stn 5, CH-1015 Lausanne, Switzerland.
   Moreau, Vincent, Ecole Polytech Fed Lausanne, Lab Environm \& Urban Econ, BP2133,Stn 16, CH-1015 Lausanne, Switzerland.
   Moreau, Vincent, Ecole Polytech Fed Lausanne, Coll Humanities, CM 2267,Stn 10, CH-1015 Lausanne, Switzerland.
   Vuille, Francois, Ecole Polytech Fed Lausanne, Energy Ctr, BAC 104,Stn 5, CH-1015 Lausanne, Switzerland.}},
DOI = {{10.1016/j.apenergy.2018.01.044}},
ISSN = {{0306-2619}},
EISSN = {{1872-9118}},
Keywords = {{Decoupling; Energy intensity; Deindustrialization; Embodied energy;
   Index decomposition analysis; Switzerland}},
Keywords-Plus = {{INDEX DECOMPOSITION ANALYSIS; ENVIRONMENTAL IMPACTS;
   INTERNATIONAL-TRADE; CO2 EMISSIONS; CONSUMPTION; PERSPECTIVE; AUSTRIA;
   FLOWS}},
Research-Areas = {{Energy \& Fuels; Engineering}},
Web-of-Science-Categories  = {{Energy \& Fuels; Engineering, Chemical}},
Author-Email = {{vincent.moreau@epfl.ch
   f.vuille@epfl.ch}},
ORCID-Numbers = {{Moreau, Vincent/0000-0002-2887-3976}},
Funding-Acknowledgement = {{College of Humanities at EPFL}},
Funding-Text = {{The authors want to thank three anonymous reviewers as well as the
   editors for their valuable comments on an earlier version of this
   article. They also thank their colleagues at EPFL's Energy Center for
   fruitful discussions on its content and methodology. Vincent Moreau
   thanks the College of Humanities at EPFL for funding under the Special
   Energy Fund.}},
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Number-of-Cited-References = {{42}},
Times-Cited = {{38}},
Usage-Count-Last-180-days = {{2}},
Usage-Count-Since-2013 = {{8}},
Journal-ISO = {{Appl. Energy}},
Doc-Delivery-Number = {{GB3RG}},
Unique-ID = {{ISI:000428974500006}},
OA = {{Other Gold}},
DA = {{2020-08-06}},
}

@article{ ISI:000428600200021,
Author = {Xue, Jiaqing and Li, Jianping and Sun, Cheng and Zhao, Sen and Mao,
   Jiangyu and Dong, Di and Li, Yanjie and Feng, Juan},
Title = {{Decadal-scale teleconnection between South Atlantic SST and southeast
   Australia surface air temperature in austral summer}},
Journal = {{CLIMATE DYNAMICS}},
Year = {{2018}},
Volume = {{50}},
Number = {{7-8}},
Pages = {{2687-2703}},
Month = {{APR}},
Abstract = {{Austral summer (December-February) surface air temperature over
   southeast Australia (SEA) is found to be remotely influenced by sea
   surface temperature (SST) in the South Atlantic at decadal time scales.
   In austral summer, warm SST anomalies in the southwest South Atlantic
   induce concurrent above-normal surface air temperature over SEA. This
   decadal-scale teleconnection occurs through the eastward propagating
   South Atlantic-Australia (SAA) wave train triggered by SST anomalies in
   the southwest South Atlantic. The excitation of the SAA wave train is
   verified by forcing experiments based on both linear barotropic and
   baroclinic models, propagation pathway and spatial scale of the observed
   SAA wave train are further explained by the Rossby wave ray tracing
   analysis in non-uniform basic flow. The SAA wave train forced by
   southwest South Atlantic warming is characterized by an anomalous
   anticyclone off the eastern coast of the Australia. Temperature
   diagnostic analyses based on the thermodynamic equation suggest
   anomalous northerly flows on western flank of this anticyclone can
   induce low-level warm advection anomaly over SEA, which thus lead to the
   warming of surface air temperature there. Finally, SST-forced
   atmospheric general circulation model ensemble experiments also
   demonstrate that SST forcing in the South Atlantic is associated with
   the SAA teleconnection wave train in austral summer, this wave train
   then modulate surface air temperature over SEA on decadal timescales.
   Hence, observations combined with numerical simulations consistently
   demonstrate the decadal-scale teleconnection between South Atlantic SST
   and summertime surface air temperature over SEA.}},
Publisher = {{SPRINGER}},
Address = {{233 SPRING ST, NEW YORK, NY 10013 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Li, JP; Sun, C (Corresponding Author), Beijing Normal Univ, State Key Lab Earth Surface Proc \& Resource Ecol, Beijing 100875, Peoples R China.
   Li, JP; Sun, C (Corresponding Author), Beijing Normal Univ, Coll Global Change \& Earth Syst Sci, Beijing 100875, Peoples R China.
   Li, JP (Corresponding Author), Qingdao Natl Lab Marine Sci \& Technol, Lab Reg Oceanog \& Numer Modeling, Qingdao 266237, Peoples R China.
   Xue, Jiaqing; Mao, Jiangyu; Dong, Di; Li, Yanjie, Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci \& Geop, Beijing 100029, Peoples R China.
   Xue, Jiaqing; Dong, Di, Univ Chinese Acad Sci, Coll Earth Sci, Beijing 100049, Peoples R China.
   Li, Jianping; Sun, Cheng; Feng, Juan, Beijing Normal Univ, State Key Lab Earth Surface Proc \& Resource Ecol, Beijing 100875, Peoples R China.
   Li, Jianping; Sun, Cheng; Feng, Juan, Beijing Normal Univ, Coll Global Change \& Earth Syst Sci, Beijing 100875, Peoples R China.
   Li, Jianping, Qingdao Natl Lab Marine Sci \& Technol, Lab Reg Oceanog \& Numer Modeling, Qingdao 266237, Peoples R China.
   Zhao, Sen, Nanjing Univ Informat Sci \& Technol, Minist Educ, Key Lab Meteorol Disaster, Nanjing 210044, Jiangsu, Peoples R China.
   Zhao, Sen, Nanjing Univ Informat Sci \& Technol, Coll Atmospher Sci, Nanjing 210044, Jiangsu, Peoples R China.
   Zhao, Sen, Univ Hawaii Manoa, Dept Atmospher Sci, Honolulu, HI 96822 USA.}},
DOI = {{10.1007/s00382-017-3764-0}},
ISSN = {{0930-7575}},
EISSN = {{1432-0894}},
Keywords = {{South Atlantic decadal variability; South Atlantic-Australia wave train;
   Southeast Australia; Surface air temperature decadal variability}},
Keywords-Plus = {{NORTH-ATLANTIC; MULTIDECADAL VARIABILITY; ATMOSPHERIC RESPONSE; COUPLED
   VARIABILITY; HEAT WAVES; RAINFALL; CLIMATE; OSCILLATION; CIRCULATION;
   MODES}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{ljp@bnu.edu.cn
   scheng@bnu.edu.cn}},
ResearcherID-Numbers = {{Sun, Cheng/O-7918-2015
   Li, Yanjie/J-3539-2019
   Mao, Jiangyu/AAJ-5420-2020
   Zhao, Sen/S-3113-2016
   Li, Jianping/I-2661-2012
   }},
ORCID-Numbers = {{Sun, Cheng/0000-0003-0474-7593
   Zhao, Sen/0000-0002-5597-1109
   Li, Jianping/0000-0003-0625-1575
   Li, Yanjie/0000-0001-6091-0303}},
Funding-Acknowledgement = {{MOST Key Project {[}2016YFA0601801]; SOA International Cooperation
   Program on Global Change and Air-Sea Interactions {[}GASI-IPOVAI-03,
   GASI-IPOVAI-06]}},
Funding-Text = {{The authors wish to thank Prof. Masahiro Watanabe for helpful
   suggestions in running the linear baroclinic model and anonymous
   reviewers for their constructive comments that significantly improved
   the quality of this paper. This work was jointly sponsored by MOST Key
   Project (2016YFA0601801) and SOA International Cooperation Program on
   Global Change and Air-Sea Interactions (GASI-IPOVAI-03, GASI-IPOVAI-06).}},
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Times-Cited = {{6}},
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DA = {{2020-08-06}},
}

@article{ ISI:000428600200031,
Author = {Frederiksen, Carsten S. and Ying, Kairan and Grainger, Simon and Zheng,
   Xiaogu},
Title = {{Modes of interannual variability in northern hemisphere winter
   atmospheric circulation in CMIP5 models: evaluation, projection and role
   of external forcing}},
Journal = {{CLIMATE DYNAMICS}},
Year = {{2018}},
Volume = {{50}},
Number = {{7-8}},
Pages = {{2845-2865}},
Month = {{APR}},
Abstract = {{Models from the coupled model intercomparison project phase 5 (CMIP5)
   dataset are evaluated for their ability to simulate the dominant slow
   modes of interannual variability in the Northern Hemisphere atmospheric
   circulation 500 hPa geopotential height in the twentieth century. A
   multi-model ensemble of the best 13 models has then been used to
   identify the leading modes of interannual variability in components
   related to (1) intraseasonal processes; (2) slowly-varying internal
   dynamics; and (3) the slowly-varying response to external changes in
   radiative forcing. Modes in the intraseasonal component are related to
   intraseasonal variability in the North Atlantic, North Pacific and North
   American, and Eurasian regions and are little affected by the larger
   radiative forcing of the Representative Concentration Pathways 8.5
   (RCP8.5) scenario. The leading modes in the slow-internal component are
   related to the El Nio-Southern Oscillation, Pacific North American or
   Tropical Northern Hemisphere teleconnection, the North Atlantic
   Oscillation, and the Western Pacific teleconnection pattern. While the
   structure of these slow-internal modes is little affected by the larger
   radiative forcing of the RCP8.5 scenario, their explained variance
   increases in the warmer climate. The leading mode in the slow-external
   component has a significant trend and is shown to be related
   predominantly to the climate change trend in the well mixed greenhouse
   gas concentration during the historical period. This mode is associated
   with increasing height in the 500 hPa pressure level. A secondary
   influence on this mode is the radiative forcing due to stratospheric
   aerosols associated with volcanic eruptions. The second slow-external
   mode is shown to be also related to radiative forcing due to
   stratospheric aerosols. Under RCP8.5 there is only one slow-external
   mode related to greenhouse gas forcing with a trend over four times the
   historical trend.}},
Publisher = {{SPRINGER}},
Address = {{233 SPRING ST, NEW YORK, NY 10013 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Frederiksen, CS (Corresponding Author), Bur Meteorol, Melbourne, Vic, Australia.
   Frederiksen, CS (Corresponding Author), Monash Univ, Sch Earth Atmosphere \& Environm, Clayton, Vic, Australia.
   Ying, KR (Corresponding Author), Chinese Acad Sci, Inst Atmospher Phys, CAS Key Lab Reg Climate Environm Res Temperate Ea, Beijing, Peoples R China.
   Frederiksen, Carsten S.; Grainger, Simon, Bur Meteorol, Melbourne, Vic, Australia.
   Frederiksen, Carsten S., Monash Univ, Sch Earth Atmosphere \& Environm, Clayton, Vic, Australia.
   Ying, Kairan; Zheng, Xiaogu, Chinese Acad Sci, Inst Atmospher Phys, CAS Key Lab Reg Climate Environm Res Temperate Ea, Beijing, Peoples R China.}},
DOI = {{10.1007/s00382-017-3776

path: /data/wos_io/savedrecs (3).bib

license_type: permissive

branch_name: refs/heads/master

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filename: savedrecs (3).bib