text:
STERDAM, NETHERLANDS}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Hu, JG (Corresponding Author), Nanjing Univ Informat Sci \& Technol, Coll Atmospher Sci, 219 Ningliu Rd, Nanjing 210044, Jiangsu, Peoples R China.
   Hu, Jinggao; Ren, Rongcai, Nanjing Univ Informat Sci \& Technol, Joint Int Res Lab Climate \& Environm Change ILCEC, Collaborat Innovat Ctr Forecast \& Evaluat Meteoro, Minist Educ KLME,Key Lab Meteorol Disaster, Nanjing, Jiangsu, Peoples R China.
   Hu, Jinggao; Ren, Rongcai, Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci \& Geop, Beijing, Peoples R China.}},
DOI = {{10.1016/j.dynatmoce.2018.07.004}},
ISSN = {{0377-0265}},
EISSN = {{1872-6879}},
Keywords = {{Stratospheric final warming; Spring season; Indian summer monsoon; Onset
   process}},
Keywords-Plus = {{ATMOSPHERIC CIRCULATION ANOMALIES; ARCTIC OSCILLATION SIGNATURE; COLD
   SEASON VARIABILITY; INTERANNUAL VARIABILITY; DOWNWARD PROPAGATION; PART
   I; RAINFALL; ENSO; TELECONNECTION; PREDICTION}},
Research-Areas = {{Geochemistry \& Geophysics; Meteorology \& Atmospheric Sciences;
   Oceanography}},
Web-of-Science-Categories  = {{Geochemistry \& Geophysics; Meteorology \& Atmospheric Sciences;
   Oceanography}},
Author-Email = {{jinggaohu@nuist.edu.cn}},
ResearcherID-Numbers = {{REN, R.-C./I-8656-2012}},
ORCID-Numbers = {{REN, R.-C./0000-0003-2809-5462}},
Funding-Acknowledgement = {{NSFCNational Natural Science Foundation of China {[}41505034, 41675039];
   Startup Foundation for Introducing Talent of NUIST {[}2014R010]}},
Funding-Text = {{This work was supported by the NSFC Project (41505034, 41675039) and the
   Startup Foundation for Introducing Talent of NUIST (2014R010).}},
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Number-of-Cited-References = {{40}},
Times-Cited = {{0}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{10}},
Journal-ISO = {{Dyn. Atmos. Oceans}},
Doc-Delivery-Number = {{GT6WO}},
Unique-ID = {{ISI:000444661800011}},
DA = {{2020-08-06}},
}

@article{ ISI:000444486900004,
Author = {Jin, Junghwan and Cheon, Seweon and Lee, Jungbae and Lee, Sanghwan and
   Kim, Jinsoo},
Title = {{Economic impact of overseas coal bed methane development project on
   Korean economy}},
Journal = {{ENERGY \& ENVIRONMENT}},
Year = {{2018}},
Volume = {{29}},
Number = {{6}},
Pages = {{905-918}},
Month = {{SEP}},
Abstract = {{Korea has increased its self-sufficiency in natural resources since
   2006. Accordingly, the number of overseas resource developments has also
   increased; however, the quantification of the economic impact of such
   developments is rarely studied. Therefore, we analyse the economic
   impact on the Korean economy and create a hypothetical Australian coal
   bed methane development project. As there is no overseas resource
   development sector in the Korean input-output table, we identify the
   relationships between the project and Korean industries using cost data
   and develop a project-industry relationship diagram. Next, we analyse
   the economic impacts of overseas coal bed methane development on the
   Korean economy, especially the production inducement, value added, and
   labour inducement effects. According to our results, the production
   inducement effect on the Korean economy is estimated to be 643,360
   million Korean Won annually with 1.918 of production inducement
   coefficient when Korean companies take full charge of the project.}},
Publisher = {{SAGE PUBLICATIONS LTD}},
Address = {{1 OLIVERS YARD, 55 CITY ROAD, LONDON EC1Y 1SP, ENGLAND}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Kim, J (Corresponding Author), Hanyang Univ, Dept Earth Resources \& Environm Engn, 222 Wangsimni Ro, Seoul 04763, South Korea.
   Jin, Junghwan; Cheon, Seweon; Lee, Jungbae; Lee, Sanghwan; Kim, Jinsoo, Hanyang Univ, Dept Earth Resources \& Environm Engn, 222 Wangsimni Ro, Seoul 04763, South Korea.}},
DOI = {{10.1177/0958305X18762153}},
ISSN = {{0958-305X}},
EISSN = {{2048-4070}},
Keywords = {{Coal bed methane; economic impact; input-output analysis;
   project-industry relationship; production inducement effects}},
Research-Areas = {{Environmental Sciences \& Ecology}},
Web-of-Science-Categories  = {{Environmental Studies}},
Author-Email = {{jinsookim@hanyang.ac.kr}},
ResearcherID-Numbers = {{Kim, Jinsoo/P-9559-2015}},
ORCID-Numbers = {{Kim, Jinsoo/0000-0001-6496-1714}},
Cited-References = {{Bank GC, 2006, EC POWDER RIVER BASI.
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Number-of-Cited-References = {{15}},
Times-Cited = {{1}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{2}},
Journal-ISO = {{Energy Environ.}},
Doc-Delivery-Number = {{GT4PO}},
Unique-ID = {{ISI:000444486900004}},
DA = {{2020-08-06}},
}

@article{ ISI:000444072400002,
Author = {Wang, Xin-Yue and Li, Xichen and Zhu, Jiang and Tanajura, Clemente A. S.},
Title = {{The strengthening of Amazonian precipitation during the wet season
   driven by tropical sea surface temperature forcing}},
Journal = {{ENVIRONMENTAL RESEARCH LETTERS}},
Year = {{2018}},
Volume = {{13}},
Number = {{9}},
Month = {{SEP}},
Abstract = {{Amazonian rainfall plays a critical role in the global climate system
   and the hydrological cycle. It is thus important to quantify changes in
   the Amazonian rainfall and clarify its mechanism. Previous studies
   indicate that the interannual variability of Amazonian precipitation
   could be largely attributed to variabilities in the South American
   monsoon system and the El Nino Southern Oscillation. However, the trend
   of the wet season tropical Amazonian precipitation during recent decades
   is not very well investigated. In this study, by combining both
   satellite and in situ observations, it is revealed that tropical
   Amazonian precipitation has significantly increased by similar to 180 to
   600 mm (in different datasets) in the wet season during the satellite
   era from 1979 to 2015. We then use a state-of-the-art atmospheric model
   to simulate the impact of the tropical sea surface temperatures (SSTs)
   on the precipitation changes. Results show that the multidecadal warming
   of the tropical Atlantic has contributed more than half of this
   precipitation change over the past three decades, while the east Pacific
   cooling plays a secondary role. We finally combine the simulation
   results and the reanalysis data to investigate the mechanisms of this
   process, i.e. the SST variability dramatically increases the convergence
   of the moisture transport over the Amazon region. The precipitation
   changes over the Amazon region largely impact on the local hydrological
   cycle and the ecosystem, and have important impacts on the global
   climate system by mediating the teleconnection between the Pacific and
   the Atlantic oceans. Our results show that the long-term change in the
   wet season Amazonian precipitation is important and deserves further
   investigation and discussion.}},
Publisher = {{IOP PUBLISHING LTD}},
Address = {{TEMPLE CIRCUS, TEMPLE WAY, BRISTOL BS1 6BE, ENGLAND}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Zhu, J (Corresponding Author), Chinese Acad Sci, Inst Atmospher Phys, ICCES, Beijing, Peoples R China.
   Zhu, J (Corresponding Author), Univ Chinese Acad Sci, Beijing, Peoples R China.
   Wang, Xin-Yue; Li, Xichen; Zhu, Jiang, Chinese Acad Sci, Inst Atmospher Phys, ICCES, Beijing, Peoples R China.
   Zhu, Jiang, Univ Chinese Acad Sci, Beijing, Peoples R China.
   Tanajura, Clemente A. S., Univ Fed Bahia, Inst Phys, Salvador, BA, Brazil.}},
DOI = {{10.1088/1748-9326/aadbb9}},
Article-Number = {{094015}},
ISSN = {{1748-9326}},
Keywords = {{convective precipitation; Amazon; tropical Atlantic; moisture
   convergence}},
Keywords-Plus = {{ATLANTIC CONVERGENCE ZONE; SOUTH-AMERICA; MULTIDECADAL OSCILLATION;
   INTERDECADAL VARIABILITY; CLIMATE VARIABILITY; RAINFALL; MONSOON;
   BRAZIL; SUMMER; CIRCULATION}},
Research-Areas = {{Environmental Sciences \& Ecology; Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Environmental Sciences; Meteorology \& Atmospheric Sciences}},
Author-Email = {{jzhu@mail.iap.ac.cn}},
ResearcherID-Numbers = {{Tanajura, Clemente/AAF-1816-2020}},
ORCID-Numbers = {{Tanajura, Clemente/0000-0002-3490-4302}},
Funding-Acknowledgement = {{National Key R\&D Program of China {[}2016YFC1401705]; `Belt and Road
   Climate Change and Observing' project of the Chinese Academy of Sciences}},
Funding-Text = {{This work was supported by the National Key R\&D Program of China
   (2016YFC1401705). This research is also supported by the `Belt and Road
   Climate Change and Observing' project of the Chinese Academy of
   Sciences. The observed and reanalysis datasets were downloaded from the
   International Pacific Research Center (IPRC)/Asia-Pacific Data-Research
   Center (APDRC) data portal (http://apdrc.soest.hawaii.edu/index.php).
   The reanalysis dataset (CFSR) was downloaded from the National Oceanic
   and Atmospheric Administration
   (https://www.ncdc.noaa.gov/data-access/model-data\#cfsr).}},
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Number-of-Cited-References = {{55}},
Times-Cited = {{15}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{8}},
Journal-ISO = {{Environ. Res. Lett.}},
Doc-Delivery-Number = {{GS9UJ}},
Unique-ID = {{ISI:000444072400002}},
OA = {{DOAJ Gold}},
DA = {{2020-08-06}},
}

@article{ ISI:000443683600016,
Author = {Cao, Xi and Wu, Renguang and Xiao, Xiao},
Title = {{A new perspective of intensified impact of El Nino-Southern Oscillation
   Modoki on tropical cyclogenesis over the western North Pacific around
   1990s}},
Journal = {{INTERNATIONAL JOURNAL OF CLIMATOLOGY}},
Year = {{2018}},
Volume = {{38}},
Number = {{11}},
Pages = {{4262-4275}},
Month = {{SEP}},
Abstract = {{Previous study detected an intensified impact of the El Nino-Southern
   Oscillation (ENSO) Modoki sea surface temperature (SST) anomalies on the
   tropical cyclone (TC) activity over the western North Pacific (WNP)
   after the early 1990s and attributed it to an expansion in areal
   coverage of the equatorial central Pacific (ECP) SST anomalies. This
   study identifies the contribution of SST anomalies in several other
   regions to this inter-decadal change in the relationship between ENSO
   Modoki SST and the WNP TC genesis. Before the early 1990s, the positive
   ECP SST anomalies induce an anomalous lower-level cyclone and
   consequently an increase in the TC genesis frequency over the southern
   part of the WNP, and the positive ECP and tropical Indian Ocean SST
   anomalies together induce an anomalous lower-level anticyclone and
   accordingly a decrease in the TC genesis frequency over the northern
   part of the WNP. As such, the relationship between the ECP SST and the
   WNP TC genesis frequency is weak. After the early 1990s, the positive
   ECP SST anomalies with a large areal coverage induce a large anomalous
   lower-level cyclone covering most of the WNP and thus an increase in the
   TC genesis frequency over the WNP. Meantime, the tropical northern
   Atlantic and western South Pacific SST anomalies during spring enhance
   the succeeding summer-autumn WNP atmospheric circulation response to the
   ECP SST anomalies through an Atlantic-Pacific teleconnection and a
   wind-evaporation positive feedback, respectively. This strengthens the
   relationship between the ECP SST and the WNP TC genesis frequency.}},
Publisher = {{WILEY}},
Address = {{111 RIVER ST, HOBOKEN 07030-5774, NJ USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Wu, RG (Corresponding Author), Chinese Acad Sci, Inst Atmospher Phys, Ctr Monsoon Syst Res, Bldg 40,Beichen West Rd, Beijing 100029, Peoples R China.
   Cao, Xi; Wu, Renguang, Chinese Acad Sci, Inst Atmospher Phys, Ctr Monsoon Syst Res, Bldg 40,Beichen West Rd, Beijing 100029, Peoples R China.
   Wu, Renguang, Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci \& Geop, Beijing, Peoples R China.
   Xiao, Xiao, Longquanyi Dist Meteorol Serv Chengdu, Chengdu, Sichuan, Peoples R China.}},
DOI = {{10.1002/joc.5667}},
ISSN = {{0899-8418}},
EISSN = {{1097-0088}},
Keywords = {{ENSO Modoki; intensified impact; tropical cyclone genesis; western North
   Pacific}},
Keywords-Plus = {{CYCLONE GENESIS FREQUENCY; INTERANNUAL VARIABILITY; CHINA SEA; OCEAN;
   CLIMATE; ENSO; SST; CIRCULATION; WINTER}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{renguang@mail.iap.ac.cn}},
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Number-of-Cited-References = {{41}},
Times-Cited = {{4}},
Usage-Count-Last-180-days = {{3}},
Usage-Count-Since-2013 = {{7}},
Journal-ISO = {{Int. J. Climatol.}},
Doc-Delivery-Number = {{GS5FV}},
Unique-ID = {{ISI:000443683600016}},
DA = {{2020-08-06}},
}

@article{ ISI:000443509200005,
Author = {Tsagkari, Marula and Gaona, Alexis and Gonzalez, Juan-Felipe and
   Jarvinen, Jaakko},
Title = {{The evolution of carbon dioxide emissions embodied in international
   trade in Poland: An input-output approach}},
Journal = {{ENVIRONMENTAL \& SOCIO-ECONOMIC STUDIES}},
Year = {{2018}},
Volume = {{6}},
Number = {{3}},
Pages = {{36-43}},
Month = {{SEP}},
Abstract = {{International agreements that aim to reduce carbon dioxide emissions
   have raised concerns due to the risk of carbon leakage caused by trade
   liberalization. This study aims to analyse the carbon dioxide emissions
   related to trade flows for the case of Poland, in order to further
   investigate the interrelationship between emissions and the quick
   economic growth the country has faced since 2000. The communist past,
   the quick liberalization of the economy, the trade opening, entrance to
   the EU and the intense carbon economy, are some of the characteristics
   that make Poland an interesting case. The data available data from 1996
   to 2008 were collected using the World Input-Output Database and were
   analyzed using the Input-Output method, and more concretely by
   constructing a multi-regional input-output model for the years studied.
   The findings indicate that there were substantial effects on the
   emissions of Poland that resulted from the opening of the economy and
   joining the European Union. Poland is a net importer of carbon emissions
   from other European countries; however, this phenomenon seems to be
   regulated by EU legislation. Additionally, it was shown that Polish
   imports from countries with less strict environmental policies
   significantly embody higher levels of emissions than its exports. This
   observation calls for stricter environmental regulations to avoid carbon
   leakage.}},
Publisher = {{DE GRUYTER POLAND SP ZOO}},
Address = {{BOGUMILA ZUGA 32A STR., 01-811 WARSAW, POLAND}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Tsagkari, M (Corresponding Author), Autonomous Univ Barcelona, ICTA, E-08193 Barcelona, Spain.
   Tsagkari, Marula, Autonomous Univ Barcelona, ICTA, E-08193 Barcelona, Spain.
   Gaona, Alexis; Gonzalez, Juan-Felipe; Jarvinen, Jaakko, Univ Barcelona, Sch Econ, Barcelona 08034, Spain.}},
DOI = {{10.2478/environ-2018-0021}},
ISSN = {{2354-0079}},
Keywords = {{Input-Output analysis; multi-regional model; ecological economics;
   carbon leakage}},
Keywords-Plus = {{CONSUMPTION}},
Research-Areas = {{Environmental Sciences \& Ecology}},
Web-of-Science-Categories  = {{Environmental Studies}},
Author-Email = {{marouko.tsagkari@mespom.eu}},
ResearcherID-Numbers = {{tsagkari, marula/AAT-3499-2020}},
ORCID-Numbers = {{tsagkari, marula/0000-0002-7925-3769}},
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Times-Cited = {{2}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{4}},
Journal-ISO = {{Environ. Socio-Econ. Stud.}},
Doc-Delivery-Number = {{GS3LO}},
Unique-ID = {{ISI:000443509200005}},
OA = {{DOAJ Gold}},
DA = {{2020-08-06}},
}

@article{ ISI:000443127200007,
Author = {Iwamura, Takuya and de Waroux, Yann le Polain and Mascia, Michael B.},
Title = {{Considering people in systematic conservation planning: insights from
   land system science}},
Journal = {{FRONTIERS IN ECOLOGY AND THE ENVIRONMENT}},
Year = {{2018}},
Volume = {{16}},
Number = {{7}},
Pages = {{388-396}},
Month = {{SEP}},
Abstract = {{Species and ecosystems worldwide continue to decline and disappear in
   spite of decades of investment in conservation efforts. Systematic
   conservation planning (SCP) is a field of study designed to improve
   conservation programs by identifying land configurations that, if
   protected, would most efficiently sustain biodiversity. Despite
   contributing to species persistence in landscapes, SCP has been
   criticized for replacing site-based conservation plans that often
   consider social context. In contrast, land system science (LSS), an
   emerging field that explores the process of land-use and land-cover
   change, integrates social systems and processes into conservation
   analyses. We suggest that by incorporating insights from LSS on social
   processes (eg livelihood adaptation or agricultural intensification),
   SCP can enhance the legitimacy of conservation plans, thereby reducing
   the gap between conservation planning and implementation. This
   represents a necessary first step for SCP to reinvent itself as a
   decision-support tool that helps to reconcile the long-standing divide
   between landscape-level species conservation and social needs.}},
Publisher = {{WILEY}},
Address = {{111 RIVER ST, HOBOKEN 07030-5774, NJ USA}},
Type = {{Review}},
Language = {{English}},
Affiliation = {{Iwamura, T (Corresponding Author), Tel Aviv Univ, Sch Zool, Fac Life Sci, Tel Aviv, Israel.
   Iwamura, Takuya, Tel Aviv Univ, Sch Zool, Fac Life Sci, Tel Aviv, Israel.
   de Waroux, Yann le Polain, McGill Univ, Inst Study Int Dev, Montreal, PQ, Canada.
   de Waroux, Yann le Polain, McGill Univ, Dept Geog, Montreal, PQ, Canada.
   Mascia, Michael B., Moore Ctr Sci, Conservat Int, Arlington, VA USA.}},
DOI = {{10.1002/fee.1824}},
ISSN = {{1540-9295}},
EISSN = {{1540-9309}},
Keywords-Plus = {{MARINE PROTECTED AREAS; TROPICAL DEFORESTATION; ECONOMIC-GEOGRAPHY;
   BRAZILIAN AMAZON; COVER CHANGE; BIODIVERSITY; GOVERNANCE;
   SUSTAINABILITY; GLOBALIZATION; BIOLOGY}},
Research-Areas = {{Environmental Sciences \& Ecology}},
Web-of-Science-Categories  = {{Ecology; Environmental Sciences}},
Author-Email = {{takuya@tauex.tau.ac.il}},
ResearcherID-Numbers = {{Mascia, Michael B./X-5516-2018
   Iwamura, Takuya/D-1125-2018
   le Polain, Yann/N-2554-2016}},
ORCID-Numbers = {{Mascia, Michael B./0000-0002-9874-9778
   Iwamura, Takuya/0000-0002-3740-7758
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Number-of-Cited-References = {{64}},
Times-Cited = {{2}},
Usage-Count-Last-180-days = {{3}},
Usage-Count-Since-2013 = {{30}},
Journal-ISO = {{Front. Ecol. Environ.}},
Doc-Delivery-Number = {{GR9WJ}},
Unique-ID = {{ISI:000443127200007}},
DA = {{2020-08-06}},
}

@article{ ISI:000442433200008,
Author = {Chen, Xianyao and Tung, Ka-Kit},
Title = {{Global-mean surface temperature variability: space-time perspective from
   rotated EOFs}},
Journal = {{CLIMATE DYNAMICS}},
Year = {{2018}},
Volume = {{51}},
Number = {{5-6}},
Pages = {{1719-1732}},
Month = {{SEP}},
Abstract = {{The observed global-mean surface temperature (GST) has been warming in
   the presence of increasing atmospheric concentration of greenhouse
   gases, but its rise has not been monotonic. Attention has increasingly
   been focused on the prominent variations about the linear trend in GST,
   especially on interdecadal and multidecadal time scales. When the
   sea-surface temperature (SST) and the land- plus-ocean surface
   temperature (ST) are averaged globally to yield the global-mean SST
   (GSST) and the GST, respectively, spatial information is lost.
   Information on both space and time is needed to properly identify the
   modes of variability on interannual, decadal, interdecadal and
   multidecadal time scales contributing to the GSST and GST variability.
   Empirical Orthogonal Function (EOF) analysis is usually employed to
   extract the space-time modes of climate variability. Here we use the
   method of pair-wise rotation of the principal components (PCs) to
   extract the modes in these time-scale bands and obtain global spatial
   EOFs that correspond closely with regionally defined climate modes.
   Global averaging these clearly identified global modes allows us to
   reconstruct GSST and GST, and in the process identify their components.
   The results are: Pacific contributes to the global mean variation mostly
   on the interannual time scale through El Nino-Southern Oscillation
   (ENSO) and its teleconnections, while the Atlantic contributes strongly
   to the global mean on the multidecadal time scale through the
   interhemispheric mode called the Atlantic Multidecadal Oscillation
   (AMO). The Pacific Decadal Oscillation (PDO) has twice as large a
   variance as the AMO, but its contribution to GST is only 1/10 that of
   the AMO because of its compensating patterns of cold and warm SST in
   northwest and northeast Pacific. Its teleconnection pattern, the
   Pacific/North America (PNA) pattern over land, is also found to be
   self-cancelling when globally averaged because of its alternating warm
   and cold centers. The Interdecadal Pacific Oscillation (IPO) is not a
   separate mode of variability but contains AMO and PDO. It contributes
   little to the global mean, and what it contributes is mainly through its
   AMO component. A better definition of a Pacific low-frequency
   variability is through the IPO Tripole Index (TPI), using difference of
   averaged SST in different regions of the Pacific. It also has no
   contribution to the GSST and GST due to the PDO being its main
   component.}},
Publisher = {{SPRINGER}},
Address = {{233 SPRING ST, NEW YORK, NY 10013 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Tung, KK (Corresponding Author), Univ Washington, Dept Appl Math, Seattle, WA 98195 USA.
   Chen, Xianyao, Ocean Univ China, Phys Oceanog Lab CIMST, Qingdao 266100, Peoples R China.
   Chen, Xianyao, Qingdao Natl Lab Marine Sci \& Technol, Qingdao 266100, Peoples R China.
   Tung, Ka-Kit, Univ Washington, Dept Appl Math, Seattle, WA 98195 USA.}},
DOI = {{10.1007/s00382-017-3979-0}},
ISSN = {{0930-7575}},
EISSN = {{1432-0894}},
Keywords = {{PDO; IPO; ENSO; AMO; Rotated EOF; Global-mean temperature variability}},
Keywords-Plus = {{EMPIRICAL MODE DECOMPOSITION; DECADAL MODULATION; PACIFIC; OSCILLATION;
   ENSO; CIRCULATION; AEROSOLS; RAINFALL; TRENDS; SERIES}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{ktung@uw.edu}},
ORCID-Numbers = {{Tung, Ka-Kit/0000-0001-8667-7167}},
Funding-Acknowledgement = {{National Science FoundationNational Science Foundation (NSF)
   {[}AGS-1262231, DMS-236 940342]; Natural Science Foundation of
   ChinaNational Natural Science Foundation of China {[}41776032, 41521091,
   U1406401]}},
Funding-Text = {{KKT was supported by National Science Foundation, under AGS-1262231 and
   DMS-236 940342. XC was supported by the Natural Science Foundation of
   China under Grant 41776032 and 41521091 and the Natural Science
   Foundation of China-Shandong Joint Fund for Marine Science Research
   Centers under Grant U1406401.}},
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Number-of-Cited-References = {{47}},
Times-Cited = {{11}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{13}},
Journal-ISO = {{Clim. Dyn.}},
Doc-Delivery-Number = {{GR2SQ}},
Unique-ID = {{ISI:000442433200008}},
OA = {{Other Gold}},
DA = {{2020-08-06}},
}

@article{ ISI:000442433200027,
Author = {Herold, N. and Santoso, A.},
Title = {{Indian Ocean warming during peak El Nio cools surrounding land masses}},
Journal = {{CLIMATE DYNAMICS}},
Year = {{2018}},
Volume = {{51}},
Number = {{5-6}},
Pages = {{2097-2112}},
Month = {{SEP}},
Abstract = {{Understanding the interactions between the Pacific and other ocean
   basins during extreme phases of the El Nio-Southern Oscillation (ENSO)
   is necessary for explaining its global climate impacts. Here climate
   model experiments are used to highlight a mechanism by which the
   characteristic warming of the Indian Ocean during peak El Nio months can
   cool North Africa and South Asia, an area encompassing over three
   billion people. It is found that warming of the Indian Ocean during
   extreme El Nio events leads to broader upper tropospheric geopotential
   height anomalies than would otherwise occur. This weakens the
   extratropical Rossby wave response initiated in the tropics and leads to
   higher pressure and reduced cloud forcing over North Africa and South
   Asia. Reanalysis data provides empirical support for this mechanism,
   although it is likely only to be prominent during strong El Nio events
   when Indian Ocean warming tends to be larger. This dampening effect
   needs to be taken into account in understanding the climatic impact of
   extreme El Nio events, which are projected to increase under global
   warming.}},
Publisher = {{SPRINGER}},
Address = {{ONE NEW YORK PLAZA, SUITE 4600, NEW YORK, NY, UNITED STATES}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Herold, N (Corresponding Author), Univ New South Wales, Climate Change Res Ctr, Sydney, NSW, Australia.
   Herold, N (Corresponding Author), Univ New South Wales, ARC Ctr Excellence Climate Syst Sci, Sydney, NSW, Australia.
   Herold, N.; Santoso, A., Univ New South Wales, Climate Change Res Ctr, Sydney, NSW, Australia.
   Herold, N.; Santoso, A., Univ New South Wales, ARC Ctr Excellence Climate Syst Sci, Sydney, NSW, Australia.
   Santoso, A., CSIRO Oceans \& Atmosphere, CSHOR, Hobart, Tas 7004, Australia.}},
DOI = {{10.1007/s00382-017-4001-6}},
ISSN = {{0930-7575}},
EISSN = {{1432-0894}},
Keywords = {{El Nino; ENSO; Indian Ocean; Teleconnection}},
Keywords-Plus = {{SST ANOMALIES; ENSO; NINO; TEMPERATURE; PACIFIC; CLIMATE; IMPACTS;
   DIPOLE; TELECONNECTIONS; VARIABILITY}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{nicholas.herold@unsw.edu.au}},
ResearcherID-Numbers = {{Santoso, Agus/P-1918-2019
   Santoso, Agus/J-7350-2012}},
ORCID-Numbers = {{Santoso, Agus/0000-0001-7749-8124
   Santoso, Agus/0000-0001-7749-8124}},
Funding-Acknowledgement = {{Australian Research CouncilAustralian Research Council {[}CE110001028];
   Australian Research CouncilAustralian Research Council; Earth Science
   and Climate Change Hub of the Australian Government's National
   Environmental Science Programme (NESP); Australian GovernmentAustralian
   Government}},
Funding-Text = {{The authors would like to thank T. Loughran for providing ACCESS model
   output and V. Dixit for discussions on aqua-planet simulations. NH is
   supported by Australian Research Council Grant CE110001028. AS is
   supported by the Australian Research Council and the Earth Science and
   Climate Change Hub of the Australian Government's National Environmental
   Science Programme (NESP). This research/project was undertaken with the
   assistance of resources and services from the National Computational
   Infrastructure (NCI), which is supported by the Australian Government.
   The NCAR Command Language (UCAR/NCAR/CISL/VETS 2016) was used to create
   figures and process data. The University of Delaware terrestrial air
   temperature data was provided by the NOAA/OAR/ESRL PSD, Boulder,
   Colorado, USA, from their Web site at http://www.esrl.noaa.gov/psd/.}},
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Number-of-Cited-References = {{49}},
Times-Cited = {{2}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{2}},
Journal-ISO = {{Clim. Dyn.}},
Doc-Delivery-Number = {{GR2SQ}},
Unique-ID = {{ISI:000442433200027}},
DA = {{2020-08-06}},
}

@article{ ISI:000442433200028,
Author = {Chen, Ruidan and Wen, Zhiping and Lu, Riyu},
Title = {{Interdecadal change on the relationship between the mid-summer
   temperature in South China and atmospheric circulation and sea surface
   temperature}},
Journal = {{CLIMATE DYNAMICS}},
Year = {{2018}},
Volume = {{51}},
Number = {{5-6}},
Pages = {{2113-2126}},
Month = {{SEP}},
Abstract = {{South China suffers from high temperature frequently in mid-summer and
   this study aims to explore the interdecadal change of interannual
   variation of the mid-summer temperature in South China. It is revealed
   that the relationship between South China temperature and atmospheric
   circulation and sea surface temperature anomaly (SSTA) experiences an
   interdecadal change around the early 1990s. Before the early 1990s,
   warmer summer in South China is associated with the mid-latitude
   teleconnection featured by higher pressure over the Ural Mountains and
   the Korean Peninsula and lower pressure around the Lake Baikal. South
   China is located at the southern flank of an anomalous high pressure.
   After the early 1990s, South China temperature is prominently influenced
   by the tropical SSTA, and meanwhile the mid-latitude teleconnection
   becomes much weaker. Warmer summer is associated with higher pressure
   centered over South China and the El Nio to La Nia transition phase. The
   higher pressure influencing South China is located more southwards after
   the early 1990s, and it is favored by the tropical SSTA. The warmer SST
   in summer over the western tropical Pacific enhances the local
   convection and triggers an anomalous local Hadley cell with stronger
   subsidence over South China, directly leading to higher pressure over
   South China. Moreover, the colder SST over the central-eastern Pacific
   induces an anomalous Walker circulation and further strengthens the
   convection over the western tropical Pacific, exerting an indirect
   impact on the higher pressure over South China. The relative role of the
   western Pacific warming and central-eastern Pacific cooling is verified
   by CAM4 simulations. The intimate relationship between the tropical SSTA
   and South China temperature occurs during the El Nio to La Nia
   transition phase, which is the case after the early 1990s and suggests
   higher predictability for South China temperature in the recent decades.}},
Publisher = {{SPRINGER}},
Address = {{233 SPRING ST, NEW YORK, NY 10013 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Chen, RD (Corresponding Author), Sun Yat Sen Univ, Sch Atmospher Sci, Ctr Monsoon \& Environm Res, Guangdong Prov Key Lab Climate Change \& Nat Disas, Guangzhou 510275, Guangdong, Peoples R China.
   Chen, RD (Corresponding Author), Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci \& Geop, Beijing 100029, Peoples R China.
   Chen, RD (Corresponding Author), Jiangsu Collaborat Innovat Ctr Climate Change, Nanjing, Jiangsu, Peoples R China.
   Chen, Ruidan, Sun Yat Sen Univ, Sch Atmospher Sci, Ctr Monsoon \& Environm Res, Guangdong Prov Key Lab Climate Change \& Nat Disas, Guangzhou 510275, Guangdong, Peoples R China.
   Wen, Zhiping, Fudan Univ, Inst Atmospher Sci, Shanghai, Peoples R China.
   Chen, Ruidan; Lu, Riyu, Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci \& Geop, Beijing 100029, Peoples R China.
   Lu, Riyu, Univ Chinese Acad Sci, Beijing 100049, Peoples R China.
   Chen, Ruidan; Wen, Zhiping, Jiangsu Collaborat Innovat Ctr Climate Change, Nanjing, Jiangsu, Peoples R China.}},
DOI = {{10.1007/s00382-017-4002-5}},
ISSN = {{0930-7575}},
EISSN = {{1432-0894}},
Keywords = {{Interdecadal change; Interannual variation; Mid-summer temperature;
   South China}},
Keywords-Plus = {{SUMMER RAINFALL; EAST; VARIABILITY; ASSOCIATION; CLIMATE}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{chenrd3@mail.sysu.edu.cn}},
Funding-Acknowledgement = {{National Key R\&D Program of China {[}2016YFA0600601]; National Natural
   Science Foundation of ChinaNational Natural Science Foundation of China
   {[}41605027, 41530530, 41320104007]}},
Funding-Text = {{This work is jointly supported by National Key R\&D Program of China
   (2016YFA0600601), National Natural Science Foundation of China (Grant
   Nos. 41605027, 41530530 and 41320104007).}},
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Number-of-Cited-References = {{33}},
Times-Cited = {{4}},
Usage-Count-Last-180-days = {{2}},
Usage-Count-Since-2013 = {{24}},
Journal-ISO = {{Clim. Dyn.}},
Doc-Delivery-Number = {{GR2SQ}},
Unique-ID = {{ISI:000442433200028}},
DA = {{2020-08-06}},
}

@article{ ISI:000442433200039,
Author = {Mukhin, Dmitry and Gavrilov, Andrey and Loskutov, Evgeny and Feigin,
   Alexander and Kurths, Juergen},
Title = {{Nonlinear reconstruction of global climate leading modes on decadal
   scales}},
Journal = {{CLIMATE DYNAMICS}},
Year = {{2018}},
Volume = {{51}},
Number = {{5-6}},
Pages = {{2301-2310}},
Month = {{SEP}},
Abstract = {{A nonlinear decomposition method is applied to the analysis of global
   sea surface temperature (SST) time series in different epochs related to
   the Pacific Decadal Oscillation (PDO) since the end of 19th century to
   present time. This method allows one to extract an optimal (small)
   number of global nonlinear teleconnection patterns associated with
   distinct dominant time scales from the original high-dimensional
   spatially extended data set. In particular, it enables us to reveal ENSO
   teleconnection patterns corresponding to different PDO cycles during the
   last 145 years, to uncover four climate shifts connected with PDO phase
   changes and to reconstruct the corresponding global PDO patterns. We
   find that SST teleconnections between the ENSO region, extra-tropical
   Pacific regions and the Indian ocean became fundamentally nonlinear
   since the second half of 20th century.}},
Publisher = {{SPRINGER}},
Address = {{233 SPRING ST, NEW YORK, NY 10013 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Mukhin, D (Corresponding Author), RAS, Inst Appl Phys, 46 Ulyanov St, Nizhnii Novgorod 603950, Russia.
   Mukhin, Dmitry; Gavrilov, Andrey; Loskutov, Evgeny; Feigin, Alexander, RAS, Inst Appl Phys, 46 Ulyanov St, Nizhnii Novgorod 603950, Russia.
   Kurths, Juergen, Potsdam Inst Climate Impact Res, Telegraphenberg A 31, D-14473 Potsdam, Germany.}},
DOI = {{10.1007/s00382-017-4013-2}},
ISSN = {{0930-7575}},
EISSN = {{1432-0894}},
Keywords = {{Climate modes; Nonlinear data decomposition; Teleconnection patterns;
   Climate shifts; Pacific decadal oscillation}},
Keywords-Plus = {{DIMENSIONALITY REDUCTION; EL-NINO; VARIABILITY; TELECONNECTIONS;
   PACIFIC; DYNAMICS}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{mukhin@ipfran.ru}},
ResearcherID-Numbers = {{Feigin, Alexander M./K-3857-2018
   Gavrilov, Andrey/T-8996-2017
   Loskutov, Evgeny/R-8263-2016
   Mukhin, Dmitry/U-1058-2017}},
ORCID-Numbers = {{Feigin, Alexander M./0000-0002-9106-7766
   Gavrilov, Andrey/0000-0001-9779-7308
   Loskutov, Evgeny/0000-0002-1648-2839
   Mukhin, Dmitry/0000-0002-5669-0771}},
Funding-Acknowledgement = {{Government of Russian Federation {[}14.Z50.31.0033]; Government of
   Russian Federation (Institute of Applied Physics of RAS); Russian
   Science FoundationRussian Science Foundation (RSF) {[}16-12-10198]}},
Funding-Text = {{The results (Sect. 3, 4, 5) were obtained and analyzed under support of
   the Government of Russian Federation (Agreement \#14.Z50.31.0033 with
   the Institute of Applied Physics of RAS). The methods (Sect. 2) were
   developed under support of the Russian Science Foundation (Grant
   \#16-12-10198).}},
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Number-of-Cited-References = {{28}},
Times-Cited = {{0}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{3}},
Journal-ISO = {{Clim. Dyn.}},
Doc-Delivery-Number = {{GR2SQ}},
Unique-ID = {{ISI:000442433200039}},
DA = {{2020-08-06}},
}

@article{ ISI:000441789600012,
Author = {Mair, Simon and Druckman, Angela and Jackson, Tim},
Title = {{Investigating fairness in global supply chains: applying an extension of
   the living wage to the Western European clothing supply chain}},
Journal = {{INTERNATIONAL JOURNAL OF LIFE CYCLE ASSESSMENT}},
Year = {{2018}},
Volume = {{23}},
Number = {{9}},
Pages = {{1862-1873}},
Month = {{SEP}},
Abstract = {{Purpose This paper explores the issue of fairness in global supply
   chains. Taking the Western European clothing supply chain as a case
   study, we demonstrate how applying a normative indicator in Social Life
   Cycle Assessment (SLCA) can contribute academic and practical insights
   into debates on fairness. To do so, we develop a new indicator that
   addresses some of the limitations of the living wage for SLCA.
   Methods We extend the standard form of living wage available for
   developing countries to include income tax and social security
   contributions. We call this extension `living labour compensation'.
   Using publically available data, we estimate net living wages, gross
   living wages, and living labour compensation rates for Brazil, Russia,
   India, and China (BRIC) in 2005. We then integrate living labour
   compensation rates into an input-output framework, which we use to
   compare living labour compensation and actual labour compensation in the
   BRIC countries in the Western European clothing supply chain in 2005.
   Results and discussion We find that in 2005, actual labour compensation
   in the Western European clothing supply chain was around half of the
   living labour compensation level, with the greatest difference being in
   the Agricultural sector. Therefore, we argue that BRIC pay in the
   Western European clothing supply chain was unfair. Furthermore, our
   living labour compensation estimates for BRIC in 2005 are similar to
   35\% higher than standard living wage estimates. Indeed, adding income
   taxes and employee social security contributions alone increases the
   living wage by similar to 10\%. Consequently, we argue there is a risk
   that investigations based on living wages are not using a representative
   measure of fairness from the employee's perspective and are
   substantially underestimating the cost of living wages from an
   employer's perspective. Finally, we discuss implications for retailers
   and living wage advocacy groups.
   Conclusions Living labour compensation extends the living wage,
   maintaining its strengths and addressing key weaknesses. It can be
   estimated for multiple countries from publically available data and can
   be applied in an input-output framework. Therefore, it is able to
   provide a normative assessment of fairness in complex global supply
   chains. Applying it to the Western European clothing supply chain, we
   were able to show that pay for workers in Brazil, Russia, India, and
   China is unfair, and draw substantive conclusions for practice.}},
Publisher = {{SPRINGER HEIDELBERG}},
Address = {{TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Mair, S (Corresponding Author), Univ Surrey, Ctr Environm \& Sustainabil, Guildford, Surrey, England.
   Mair, Simon; Druckman, Angela; Jackson, Tim, Univ Surrey, Ctr Environm \& Sustainabil, Guildford, Surrey, England.}},
DOI = {{10.1007/s11367-017-1390-z}},
ISSN = {{0948-3349}},
EISSN = {{1614-7502}},
Keywords = {{Clothing; Fair wage; Fairness; Fashion; Input-output analysis; Living
   wage; Social impact; Social LCA}},
Keywords-Plus = {{INCOME REFERENCE POINTS; LIFE-CYCLE ASSESSMENT; PART 1; IMPACT
   ASSESSMENT; OICONOMY PROJECT; APPAREL SECTOR; SUSTAINABILITY;
   METHODOLOGY; LEVEL; WORLD}},
Research-Areas = {{Engineering; Environmental Sciences \& Ecology}},
Web-of-Science-Categories  = {{Engineering, Environmental; Environmental Sciences}},
Author-Email = {{s.mair@surrey.ac.uk}},
ORCID-Numbers = {{Mair, Simon/0000-0001-5143-8668
   Druckman, Angela/0000-0002-2515-0369}},
Funding-Acknowledgement = {{UK's Economic and Social Research CouncilEconomic \& Social Research
   Council (ESRC) {[}ES/J500148/1]; Natural Environment Research
   CouncilNERC Natural Environment Research Council {[}ES/J500148/1];
   ESRCEconomic \& Social Research Council (ESRC) {[}ES/M010163/1]}},
Funding-Text = {{We would like to thank three anonymous reviewers for their insightful
   comments. This work was supported by a joint grant from the UK's
   Economic and Social Research Council and Natural Environment Research
   Council, grant number ES/J500148/1, and the ESRC funded Centre for the
   Understanding of Sustainable Prosperity, grant number ES/M010163/1.}},
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