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Number-of-Cited-References = {{35}},
Times-Cited = {{1}},
Usage-Count-Last-180-days = {{3}},
Usage-Count-Since-2013 = {{20}},
Journal-ISO = {{Int. J. Climatol.}},
Doc-Delivery-Number = {{GO2IT}},
Unique-ID = {{ISI:000439794000002}},
DA = {{2020-08-06}},
}

@article{ ISI:000439794000010,
Author = {Gao, Ya and Wang, Huijun and Chen, Dong},
Title = {{Precipitation anomalies in the Pan-Asian monsoon region during El Nino
   decaying summer 2016}},
Journal = {{INTERNATIONAL JOURNAL OF CLIMATOLOGY}},
Year = {{2018}},
Volume = {{38}},
Number = {{9}},
Pages = {{3618-3632}},
Month = {{JUL}},
Abstract = {{The El Nino-Southern Oscillation (ENSO) has an intimate relationship
   with Asian summer monsoon precipitation. Previous study pointed out that
   the most recent 2015-2016 El Nino event is tied with the 1997-1998 and
   1982-1983 El Nino events as the strongest event since 1950, which may
   result in catastrophe in Asian monsoon region. Therefore, in this
   article, we mainly focus on the anomalous precipitation pattern in the
   Pan-Asian monsoon region during MJJ 2016 and its impact factors. Results
   show that the summer precipitation anomalies display a meridional
   tripole pattern from north to south in the Pan-Asian monsoon region
   during 2016. This pattern indicates that the anomalous increased
   rainfall is located over the middle-lower reaches of the Yangtze River
   valley-East China Sea (ECS) and the tropical eastern Indian
   Ocean-western Maritime Continent, while the anomalous decreased rainfall
   is located over the South China Sea (SCS)-Philippine Sea. Results
   suggest that the preceding winter and spring ENSO and the simultaneous
   summer Maritime Continent sea surface temperature (SST) are the primary
   impact factors of the pattern of tripole precipitation anomalies in the
   Pan-Asian monsoon region during MJJ 2016. The preceding ENSO can
   intensify the western North Pacific subtropical high (WPSH), which
   results in the anomalous decrease in precipitation over the Indo-China
   Peninsula-Philippine Sea. Meanwhile, more moisture is transported from
   the northwestern flank of WPSH to the Yangtze River valley-ESC to
   increase rainfall. In the ENSO decaying summer, the Maritime Continent
   SST anomalous warming induces an anomalous convergence in situ, which
   increases the local precipitation. Later, this warming can intensify the
   WPSH through the local meridional circulation. The north Indian Ocean
   SST, including Arabian Sea and Bay of Bengal, also has a high
   relationship with tripole precipitation pattern, but it cannot induce
   this tripole rainfall pattern, which establishes the linkage through the
   extending WPSH.}},
Publisher = {{WILEY}},
Address = {{111 RIVER ST, HOBOKEN 07030-5774, NJ USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Gao, Y (Corresponding Author), Chinese Acad Sci, Inst Atmospher Phys, Nansen Zhu Int Res Ctr, Beijing, Peoples R China.
   Gao, Ya; Chen, Dong, Chinese Acad Sci, Inst Atmospher Phys, Nansen Zhu Int Res Ctr, Beijing, Peoples R China.
   Gao, Ya; Wang, Huijun; Chen, Dong, Nanjing Univ Informat Sci \& Technol, Collaborat Innovat Ctr Forecast \& Evaluat Meteoro, Key Lab Meteorol Disaster, Nanjing, Jiangsu, Peoples R China.}},
DOI = {{10.1002/joc.5522}},
ISSN = {{0899-8418}},
EISSN = {{1097-0088}},
Keywords = {{ENSO; Indian Ocean SST; Maritime Continent SST; precipitation anomaly in
   2016; western North Pacific subtropical high}},
Keywords-Plus = {{PRINCIPAL MODES; INDIAN-OCEAN; SST ANOMALIES; EAST; VARIABILITY; ENSO;
   SEA; TELECONNECTION; CLIMATE}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{gaoy@mail.iap.ac.cn}},
Funding-Acknowledgement = {{National Key Research and Development Program of China
   {[}2016YFA0600701]; National Natural Science Foundation of ChinaNational
   Natural Science Foundation of China {[}41505070, 41421004]; CAS-PKU
   Joint Research Program}},
Funding-Text = {{National Key Research and Development Program of China, Grant/Award
   Number: 2016YFA0600701; National Natural Science Foundation of China,
   Grant/Award Numbers: 41505070, 41421004; CAS-PKU Joint Research Program}},
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Number-of-Cited-References = {{36}},
Times-Cited = {{2}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{12}},
Journal-ISO = {{Int. J. Climatol.}},
Doc-Delivery-Number = {{GO2IT}},
Unique-ID = {{ISI:000439794000010}},
DA = {{2020-08-06}},
}

@article{ ISI:000440103200002,
Author = {Zerouali, Bilel and Mesbah, Mohamed and Chettih, Mohamed and Djemai,
   Mohammed},
Title = {{Contribution of cross time-frequency analysis in assessment of possible
   relationships between large-scale climatic fluctuations and rainfall of
   northern central Algeria}},
Journal = {{ARABIAN JOURNAL OF GEOSCIENCES}},
Year = {{2018}},
Volume = {{11}},
Number = {{14}},
Month = {{JUL}},
Abstract = {{This paper is proposed for the investigation of possible relationships
   between the large-scale atmospheric circulation phenomena such as the
   North Atlantic Oscillation (NAO), Southern Oscillation (SOI),
   Mediterranean Oscillation (MO), Western Mediterranean Oscillation (WeMO)
   and rainfall of Sebaou river watershed (Northern central Algeria),
   covering a period of 39 years at monthly scale. Several time and
   scale-based methods were used: correlation and spectral analysis (CSA),
   continuous wavelet transform (CWT), multiresolution wavelet analysis
   (MRWA), cross wavelet analysis (XWT), wavelet coherence transform (WCT)
   and cross multiresolution wavelet analysis (CMRWA). The rainfall
   analysis by CSA and CWT has been clearly demonstrating the dominance of
   1 year and 1-3-year modes, which they explain 30 to 51\% and 25 to 28\%
   of the variance respectively. However, the indices have shown that
   inter-annual fluctuations up to long-term explain between 60 and 90\%.
   CWT and MRWA indicated significant fluctuations materialising a dry
   period more marked between the 1980s and 1990s with strong trend towards
   drier conditions starting from the 1980s, explained by the decadal
   components D7 and the approximation A7. In addition to the annual
   component, the XWT spectrums reveal strong coefficients for the SOI
   between 1992-2005 and 1986-2000 for the modes of 5-10 years and higher
   than 10 years respectively and less intense for NAO. The WCT between NAO
   and rainfall indicated the most significant relationship for 1 year, 1-3
   years and 3-5 years approximately from the early 1980s corresponding to
   the dry period. However, the SOI affects rainfall only locally and with
   significant values more or less localised in the time-frequency space
   between MO, WeMO and rainfall, but this influence could be significant
   for low-frequency events. CWMRA shows that the components of 5-10 years
   and higher than 10 years are the most effective to represent climate
   index-rainfall significant relationships, where change in Daubechies
   wavelet properties can improve the correlation across the scales.
   Furthermore, has indicated that the short-term processes dominate the
   relationship index-rainfall, which masks the long-term phenomena whose
   influence can sometimes be very distant. As such, the rainfall
   variability of the study area has shown fairly significant links, at
   least locally with large-scale atmospheric circulation phenomena.}},
Publisher = {{SPRINGER HEIDELBERG}},
Address = {{TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Zerouali, B (Corresponding Author), Amar Telidji Univ, Res Lab Water Resources Soil \& Environm, Dept Civil Engn, Fac Civil Engn \& Architecture, POB 37G, Laghouat 03000, Algeria.
   Zerouali, Bilel; Chettih, Mohamed, Amar Telidji Univ, Res Lab Water Resources Soil \& Environm, Dept Civil Engn, Fac Civil Engn \& Architecture, POB 37G, Laghouat 03000, Algeria.
   Mesbah, Mohamed, Univ Sci \& Technol Houari Boumediene, Fac Earth Sci, LGBO Lab, BP 32, Bab Ezzouar 16311, Algeria.
   Djemai, Mohammed, Mouloud Mammeri Univ, Lab Geomat Environm \& Dev, Dept Civil Engn, BP 10RP, Hasnaoua, Tizi Ouzou, Algeria.}},
DOI = {{10.1007/s12517-018-3728-7}},
Article-Number = {{392}},
ISSN = {{1866-7511}},
EISSN = {{1866-7538}},
Keywords = {{Rainfall; Atmospheric circulation phenomena; Time and scale-based
   methods; Cross wavelet analysis; Sebaouriver; Algeria}},
Keywords-Plus = {{ATLANTIC OSCILLATION; ATMOSPHERIC CIRCULATION; WAVELET TRANSFORM;
   TELECONNECTION PATTERNS; SPATIOTEMPORAL ANALYSIS; SPECTRAL-ANALYSES;
   PRECIPITATION; DROUGHT; TEMPERATURE; VARIABILITY}},
Research-Areas = {{Geology}},
Web-of-Science-Categories  = {{Geosciences, Multidisciplinary}},
Author-Email = {{b.zerouali@lagh-univ.dz}},
ResearcherID-Numbers = {{Zerouali, Bilel/P-7046-2016}},
ORCID-Numbers = {{Zerouali, Bilel/0000-0003-4735-9750}},
Funding-Acknowledgement = {{Directorate General for Scientific Research and Technological
   Development}},
Funding-Text = {{The authors gratefully thank all the engineers of the ``Agence nationale
   des ressources hydriques{''}, who have provided us materials, and
   necessary data and the Directorate General for Scientific Research and
   Technological Development for supporting this research. We sincerely
   thank the reviewers for constructive criticisms and valuable comments.}},
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Number-of-Cited-References = {{69}},
Times-Cited = {{1}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{6}},
Journal-ISO = {{Arab. J. Geosci.}},
Doc-Delivery-Number = {{GO5WR}},
Unique-ID = {{ISI:000440103200002}},
DA = {{2020-08-06}},
}

@article{ ISI:000439442900004,
Author = {King, Martin P. and Herceg-Bulic, Ivana and Blade, Ileana and
   Garcia-Serrano, Javier and Keenlyside, Noel and Kucharski, Fred and Li,
   Camille and Sobolowski, Stefan},
Title = {{Importance of Late Fall ENSO Teleconnection in the Euro-Atlantic Sector}},
Journal = {{BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY}},
Year = {{2018}},
Volume = {{99}},
Number = {{7}},
Pages = {{1337-1344}},
Month = {{JUL}},
Abstract = {{Recent studies have indicated the importance of fall climate forcings
   and teleconnections in influencing the climate of the northern mid- to
   high latitudes. Here, we present some exploratory analyses using
   observational data and seasonal hindcasts, with the aim of highlighting
   the potential of the El Nino-Southern Oscillation (ENSO) as a driver of
   climate variability during boreal late fall and early winter (November
   and December) in the North Atlantic-European sector, and motivating
   further research on this relatively unexplored topic. The atmospheric
   ENSO teleconnection in November and December is reminiscent of the east
   Atlantic pattern and distinct from the well-known arching extratropical
   Rossby wave train found from January to March. Temperature and
   precipitation over Europe in November are positively correlated with the
   Nino-3.4 index, which suggests a potentially important ENSO climate
   impact during late fall. In particular, the ENSO-related temperature
   anomaly extends over a much larger area than during the subsequent
   winter months. We discuss the implications of these results and pose
   some research questions.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{King, MP (Corresponding Author), Uni Res Climate, Bergen, Norway.
   King, MP (Corresponding Author), Bjerknes Ctr Climate Res, Bergen, Norway.
   King, Martin P.; Sobolowski, Stefan, Uni Res Climate, Bergen, Norway.
   King, Martin P.; Keenlyside, Noel; Li, Camille; Sobolowski, Stefan, Bjerknes Ctr Climate Res, Bergen, Norway.
   Herceg-Bulic, Ivana, Univ Zagreb, Dept Geophys, Zagreb, Croatia.
   Blade, Ileana, Univ Barcelona, Dept Appl Phys, Grp Meteorol, Barcelona, Spain.
   Garcia-Serrano, Javier, Barcelona Supercomp Ctr, Barcelona, Spain.
   Keenlyside, Noel; Li, Camille, Univ Bergen, Geophys Inst, Bergen, Norway.
   Kucharski, Fred, Abdus Salam Int Ctr Theoret Phys, Trieste, Italy.}},
DOI = {{10.1175/BAMS-D-17-0020.1}},
ISSN = {{0003-0007}},
EISSN = {{1520-0477}},
Keywords-Plus = {{NINO-SOUTHERN OSCILLATION; SEA-SURFACE TEMPERATURES; NORTH-ATLANTIC;
   EL-NINO; ATMOSPHERIC CIRCULATION; PRECIPITATION; STRATOSPHERE; CLIMATE;
   SIMULATIONS; REGION}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{martin.king@uni.no}},
ResearcherID-Numbers = {{Garcia-Serrano, Javier/I-5058-2015
   Li, Camille/G-5802-2011
   Keenlyside, Noel S/E-8303-2013
   }},
ORCID-Numbers = {{Garcia-Serrano, Javier/0000-0003-3913-0876
   Li, Camille/0000-0002-5439-2973
   Keenlyside, Noel S/0000-0002-8708-6868
   King, Martin/0000-0002-8152-0897}},
Funding-Acknowledgement = {{Research Council of NorwayResearch Council of Norway {[}255027];
   Croatian Science Foundation {[}2831]; Spanish MINECO {[}CGL2015-68342-R]}},
Funding-Text = {{We gratefully acknowledge the National Centers for Environmental
   Prediction (NCEP)-National Center for Atmospheric Research (NCAR)
   Reanalysis 1 (R-1), ERA-Interim, E-Obs, CRU TS, Hadley Centre Sea Ice
   and Sea Surface Temperature dataset (HadISST), and ECMWF Sys4 hindcasts
   datasets. MPK, CL, and SS are partially supported by the Research
   Council of Norway's Klimaforsk program (Project 255027), IHB by the
   Croatian Science Foundation (Project 2831), and IB and JG-S by the
   Spanish MINECO-funded DANAE project (CGL2015-68342-R). Comments from Dr.
   M. A. Alexander (editor) and three reviewers have helped to improve this
   article.}},
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Number-of-Cited-References = {{35}},
Times-Cited = {{14}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{8}},
Journal-ISO = {{Bull. Amer. Meteorol. Soc.}},
Doc-Delivery-Number = {{GN8SO}},
Unique-ID = {{ISI:000439442900004}},
OA = {{Green Published}},
DA = {{2020-08-06}},
}

@article{ ISI:000438495200002,
Author = {Sun, Cheng and Li, Jianping and Li, Xiang and Xue, Jiaqing and Ding,
   Ruiqiang and Xie, Fei and Li, Yang},
Title = {{Oceanic forcing of the interhemispheric SST dipole associated with the
   Atlantic Multidecadal Oscillation}},
Journal = {{ENVIRONMENTAL RESEARCH LETTERS}},
Year = {{2018}},
Volume = {{13}},
Number = {{7}},
Month = {{JUL}},
Abstract = {{In this study, the interhemispheric sea surface temperature (SST)
   signature of the Atlantic Multidecadal Oscillation (AMO) is analyzed and
   compared between observations and slab ocean model (SOM) simulations.
   Observational analysis suggests a robust interhemispheric SST dipole
   across the Atlantic associated with the AMO, manifested by a strong
   inverse relationship between the AMO and subpolar South Atlantic decadal
   SST anomalies. None of the SOMs analyzed could reproduce the observed
   interhemispheric dipole of the AMO; instead, they consistently simulate
   an interhemispheric coherent SST pattern. In the SOMs, the North
   Atlantic decadal SST anomalies synchronize the variations of South
   Atlantic SST through a cross-hemispheric atmosphere teleconnection and
   thermodynamic processes. This discrepancy between the SOM simulations
   and the observation is possibly due to deficiencies in representing
   ocean dynamical processes. Further analyses of the fully coupled
   versions of the SOMs suggest that the observed interhemispheric dipole
   of the AMO can be reproduced only by including ocean dynamics related to
   the Atlantic meridional overturning circulation. Our findings highlight
   that the ocean dynamics play a non-negligible role and should be taken
   into consideration in better understanding the observed feature of the
   AMO.}},
Publisher = {{IOP PUBLISHING LTD}},
Address = {{TEMPLE CIRCUS, TEMPLE WAY, BRISTOL BS1 6BE, ENGLAND}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Sun, C (Corresponding Author), Beijing Normal Univ, Coll Global Change \& Earth Syst Sci GCESS, Beijing 100875, Peoples R China.
   Sun, Cheng; Li, Jianping; Xie, Fei, Beijing Normal Univ, Coll Global Change \& Earth Syst Sci GCESS, Beijing 100875, Peoples R China.
   Li, Jianping, Qingdao Natl Lab forMarine Sci \& Technol, Lab Reg Oceanog \& Numer Modeling, Qingdao 266237, Peoples R China.
   Li, Xiang, State Ocean Adm, Natl Marine Environm Forecasting Ctr, Key Lab Res Marine Hazards Forecasting, Beijing 100081, Peoples R China.
   Xue, Jiaqing; Ding, Ruiqiang, Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci \& Geop, Beijing 100029, Peoples R China.
   Xue, Jiaqing, Univ Chinese Acad Sci, Coll Earth Sci, Beijing 100049, Peoples R China.
   Li, Jianping; Li, Yang, Chengdu Univ Informat Technol, Coll Atmospher Sci, Plateau Atmosphere \& Environm Key Lab Sichuan Pro, Chengdu 610225, Sichuan, Peoples R China.}},
DOI = {{10.1088/1748-9326/aacf66}},
Article-Number = {{074026}},
ISSN = {{1748-9326}},
Keywords = {{Atlantic Multidecadal Oscillation; Atlantic meridional overturning
   circulation; ocean dynamics; interhemispheric SST dipole}},
Keywords-Plus = {{SEA-SURFACE TEMPERATURE; NORTH-ATLANTIC; THERMOHALINE CIRCULATION;
   OVERTURNING CIRCULATION; CLIMATE VARIABILITY; LAST DEGLACIATION;
   HEMISPHERE; IMPACTS; MODEL; PACIFIC}},
Research-Areas = {{Environmental Sciences \& Ecology; Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Environmental Sciences; Meteorology \& Atmospheric Sciences}},
Author-Email = {{scheng@bnu.edu.cn
   ljp@bnu.edu.cn}},
ResearcherID-Numbers = {{Sun, Cheng/O-7918-2015
   Li, Jianping/I-2661-2012
   Xie, Fei/I-9766-2016}},
ORCID-Numbers = {{Sun, Cheng/0000-0003-0474-7593
   Li, Jianping/0000-0003-0625-1575
   Xie, Fei/0000-0003-2891-3883}},
Funding-Acknowledgement = {{National Science Foundation of ChinaNational Natural Science Foundation
   of China {[}41775038, 41790474]; National Programme on Global Change and
   Air-Sea Interaction {[}GASI-IPOVAI-06, GASI-IPOVAI-03]; State Key
   Laboratory of Tropical Oceanography, South China Sea Institute of
   Oceanology, Chinese Academy of Sciences {[}LTO1801]}},
Funding-Text = {{This work was jointly supported by the National Science Foundation of
   China (41775038, 41790474), the National Programme on Global Change and
   Air-Sea Interaction (GASI-IPOVAI-06 and GASI-IPOVAI-03), and the State
   Key Laboratory of Tropical Oceanography, South China Sea Institute of
   Oceanology, Chinese Academy of Sciences (Project No. LTO1801).}},
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Number-of-Cited-References = {{64}},
Times-Cited = {{9}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{6}},
Journal-ISO = {{Environ. Res. Lett.}},
Doc-Delivery-Number = {{GM8PR}},
Unique-ID = {{ISI:000438495200002}},
OA = {{DOAJ Gold}},
DA = {{2020-08-06}},
}

@article{ ISI:000437737700002,
Author = {Kurita, Naoyuki and Horikawa, Mayumi and Kanamori, Hironari and
   Fujinami, Hatsuki and Kumagai, Tomo'omi and Kume, Tomonori and Yasunari,
   Tetsuzo},
Title = {{Interpretation of El Nino-Southern Oscillation-related precipitation
   anomalies in north-western Borneo using isotopic tracers}},
Journal = {{HYDROLOGICAL PROCESSES}},
Year = {{2018}},
Volume = {{32}},
Number = {{14}},
Pages = {{2176-2186}},
Month = {{JUL 1}},
Abstract = {{We examined rainfall anomalies associated with the El Nino-Southern
   Oscillation (ENSO) in northern Sarawak, Malaysia, using the oxygen
   isotopic composition of rainfall. Two precipitation-sampling campaigns
   were conducted for isotope analysis: (a) at the Lambir Hill National
   Park (4.2 degrees N, 114.0 degrees E) from July 2004 to October 2006 and
   (b) at the Gunung Mulu National Park (3.9 degrees N, 114.8 degrees E)
   from January 2006 to July 2008. The records from these campaigns were
   merged with a previously published rainfall isotope dataset from Gunung
   Mulu site to create a 7-year-long record of the oxygen isotopic
   composition of Sarawak rainfall. The record exhibits clear intraseasonal
   variations (ISVs) with periods ranging from 10 to 70days. The ISVs of
   10- to 90-day band-pass filtered oxygen isotopic composition are linked
   to the synoptic-scale precipitation anomalies over the southern South
   China Sea (SCS). The lead-lag correlation map of precipitation with the
   filtered oxygen isotope anomalies shows that an anomalous wet condition
   responsible for the decrease in oxygen isotopic composition appears over
   the SCS in association with the passage of north-eastward propagation of
   the boreal summer intraseasonal oscillation (BSISO) in the summer
   monsoon season. The anomalous wet condition in spring is connected with
   eastward-propagating Madden-Julian oscillation (MJO), whereas the
   sustained wet condition in winter is responsible for the occurrence of
   the Borneo vortex (BV) over the SCS. ENSO modulates the frequency of
   these synoptic conditions on a seasonal and longer time scale, showing a
   strong correlation between the seasonal isotopic anomalies and the
   Southern Oscillation index. We therefore discern, from the significant
   correlation between the isotope anomalies and area-averaged Sarawak
   rainfall anomalies (R=-0.65, p<0.01), that ENSO-related precipitation
   anomalies are linked to the seasonal modulation of the BSISO and MJO
   activity and BV genesis.}},
Publisher = {{WILEY}},
Address = {{111 RIVER ST, HOBOKEN 07030-5774, NJ USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Kurita, N (Corresponding Author), Nagoya Univ, Inst Space Earth Environm Res ISEE, Chikusa Ku, Furo Cho, Nagoya, Aichi 4648601, Japan.
   Kurita, Naoyuki; Kanamori, Hironari; Fujinami, Hatsuki; Kumagai, Tomo'omi, Nagoya Univ, Inst Space Earth Environm Res ISEE, Nagoya, Aichi, Japan.
   Horikawa, Mayumi, Nagoya Univ, Grad Sch Environm Studies, Nagoya, Aichi, Japan.
   Kumagai, Tomo'omi, Univ Tokyo, Grad Sch Agr \& Life Sci, Tokyo, Japan.
   Kume, Tomonori, Natl Taiwan Univ, Sch Forestry \& Resource Conservat, Taipei, Taiwan.
   Yasunari, Tetsuzo, Res Inst Humanity \& Nat, Kyoto, Japan.}},
DOI = {{10.1002/hyp.13164}},
ISSN = {{0885-6087}},
EISSN = {{1099-1085}},
Keywords-Plus = {{MADDEN-JULIAN OSCILLATION; SUMMER INTRASEASONAL OSCILLATIONS; EAST ASIAN
   TELECONNECTION; MARITIME CONTINENT; DIURNAL CYCLE; RAINFALL VARIABILITY;
   WINTER RAINFALL; GLOBAL TROPICS; MONSOON REGION; CHINA SEA}},
Research-Areas = {{Water Resources}},
Web-of-Science-Categories  = {{Water Resources}},
Author-Email = {{nkurita@nagoya-u.jp}},
ResearcherID-Numbers = {{Fujinami, Hatsuki/N-3968-2019
   Kurita, Naoyuki/C-6120-2014
   Kumagai, Tomo'omi/A-4791-2011
   Fujinami, Hatsuki/B-3000-2010
   Kanamori, Hironari/S-2536-2018
   }},
ORCID-Numbers = {{Fujinami, Hatsuki/0000-0002-2400-479X
   Fujinami, Hatsuki/0000-0002-2400-479X
   Kanamori, Hironari/0000-0002-9910-7806
   Kurita, Naoyuki/0000-0003-1165-0124}},
Funding-Acknowledgement = {{collaborative research program of Hydrospheric Atmospheric Research
   Center (HyARC) of Nagoya University, entitled ``Application of stable
   isotope for evaluation of multi-scale water cycle processes{''}}},
Funding-Text = {{This study was supported by collaborative research program of
   Hydrospheric Atmospheric Research Center (HyARC) of Nagoya University,
   entitled ``Application of stable isotope for evaluation of multi-scale
   water cycle processes{''}. The authors gratefully acknowledge members of
   management committee of analytical system for water isotopes at HyARC of
   Nagoya University for water isotope analysis and quality control of
   them. We also thank two anonymous reviewers for constructive comments on
   the manuscript and editor for their valuable suggestions. The data are
   available as indicated in Section 2 and otherwise from the authors upon
   request (nkurita@nagoya-u.jp).}},
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Number-of-Cited-References = {{67}},
Times-Cited = {{4}},
Usage-Count-Last-180-days = {{2}},
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Journal-ISO = {{Hydrol. Process.}},
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@article{ ISI:000437117200002,
Author = {Mura, Matteo and Longo, Mariolina and Micheli, Pietro and Bolzani,
   Daniela},
Title = {{The Evolution of Sustainability Measurement Research}},
Journal = {{INTERNATIONAL JOURNAL OF MANAGEMENT REVIEWS}},
Year = {{2018}},
Volume = {{20}},
Number = {{3, SI}},
Pages = {{661-695}},
Month = {{JUL}},
Abstract = {{Research in sustainability measurement has been growing at a very high
   pace over the past years, and it has explored a variety of issues, from
   sustainability disclosure to measurement in green supply chains, from
   the diffusion of environmental standards to the political use of
   sustainability metrics. This study is the first to report and discuss
   the results of a comprehensive review of the sustainability measurement
   literature. In particular, the authors adopt a wide conceptualization of
   the measurement process, and analyze data through a bibliometric
   method-bibliographic coupling. The results show that the literature is
   divided into eight distinct areas of inquiry and 12 sub-fields, some of
   which have expanded significantly over recent years, and others appear
   to be waning. Furthermore, the lack of a comprehensive view of
   sustainability measurement has led to the development of many separate
   communities, resulting in duplications of effort, incomplete framing of
   the problem, and the proposal of partial solutions. However, findings
   drawn in sustainability measurement research could inform current
   debates in performance measurement and management in three main ways: by
   emphasizing stakeholders' roles in the design, implementation and use of
   measures; by indicating ways to establish common measures and sharing
   data between organizations; and by adopting novel theoretical
   perspectives. Equally, future sustainability measurement studies could
   benefit from consideration of extant research on strategic performance
   measurement and on the behavioral effects of measurement practices.}},
Publisher = {{WILEY}},
Address = {{111 RIVER ST, HOBOKEN 07030-5774, NJ USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Mura, M (Corresponding Author), Univ Bologna, Dept Management, Via Terracini 28, I-40131 Bologna, Italy.
   Mura, Matteo; Longo, Mariolina, Univ Bologna, Dept Management, Via Terracini 28, I-40131 Bologna, Italy.
   Micheli, Pietro, Univ Warwick, Warwick Business Sch, Coventry CV4 7AL, W Midlands, England.
   Bolzani, Daniela, Univ Cattolica Sacro Cuore, Dept Econ \& Management Sci, Milan Via Necchi 5, I-20123 Milan, Italy.}},
DOI = {{10.1111/ijmr.12179}},
ISSN = {{1460-8545}},
EISSN = {{1468-2370}},
Keywords-Plus = {{CORPORATE SOCIAL-RESPONSIBILITY; SUPPLY CHAIN MANAGEMENT;
   PERFORMANCE-MEASUREMENT SYSTEMS; INPUT-OUTPUT-ANALYSIS; ENVIRONMENTAL
   PERFORMANCE; STAKEHOLDER INFLUENCE; VOLUNTARY DISCLOSURE;
   EMPIRICAL-ANALYSIS; CARBON FOOTPRINTS; CSR DISCLOSURE}},
Research-Areas = {{Business \& Economics}},
Web-of-Science-Categories  = {{Business; Management}},
Author-Email = {{matteo.mura@unibo.it}},
ResearcherID-Numbers = {{Micheli, Pietro/O-4851-2019
   }},
ORCID-Numbers = {{Micheli, Pietro/0000-0001-7920-6500
   MURA, MATTEO/0000-0002-5762-2228}},
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