text:
ASIAN WINTER MONSOON; SURFACE TEMPERATURE;
   WESTERN PACIFIC; COUPLED PATTERNS; ALTIMETER DATA; VARIABILITY; ENSO;
   RISE; ANOMALIES}},
Research-Areas = {{Oceanography}},
Web-of-Science-Categories  = {{Oceanography}},
Author-Email = {{jianlongf@hotmail.com}},
Funding-Acknowledgement = {{National Key Research and Development Program of China
   {[}2017YFC1404200, 2016YFC1401900]; National Natural Science Foundation
   of ChinaNational Natural Science Foundation of China {[}41706020,
   41406032]; Key Laboratory of Research on Marine Hazards Forecasting}},
Funding-Text = {{This study was supported by the National Key Research and Development
   Program of China (2017YFC1404200 and 2016YFC1401900), the National
   Natural Science Foundation of China (Grant No. 41706020 and No.
   41406032), and the Open Fund of the Key Laboratory of Research on Marine
   Hazards Forecasting.}},
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Number-of-Cited-References = {{77}},
Times-Cited = {{4}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{7}},
Journal-ISO = {{Ocean Dyn.}},
Doc-Delivery-Number = {{GD5YU}},
Unique-ID = {{ISI:000430585900005}},
DA = {{2020-08-06}},
}

@article{ ISI:000430540200008,
Author = {Yu, Lejiang and Zhong, Shiyuan and Zhou, Mingyu and Sun, Bo and
   Lenschow, Donald H.},
Title = {{Antarctic Summer Sea Ice Trend in the Context of High-Latitude
   Atmospheric Circulation Changes}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2018}},
Volume = {{31}},
Number = {{10}},
Pages = {{3909-3920}},
Month = {{MAY}},
Abstract = {{The potential mechanisms underlying the observed increasing trend in
   Antarctic summertime sea ice cover for the 1979-2017 period have been
   investigated using a relatively novel method called the self-organizing
   map (SOM). Among the nine nodes generated to explain the variability of
   Antarctic sea ice cover, two (nodes 3 and 7) exhibit a statistically
   significant linear trend in the time series of the frequency of the SOM
   pattern occurrence that together explain 40\% of the total trend in the
   sea ice cover. These two nodes have completely opposite spatial patterns
   and directions of trend and are associated with different atmospheric
   circulation patterns. Node 3, which represents an increase in sea ice
   over the Weddell Sea and the eastern Ross Sea and a decrease over the
   other coastal seas of West Antarctica, appears to be related to the
   positive phase of the southern annular mode (SAM) linked with the La
   Nina pattern of sea surface temperature (SST) over the tropical Pacific
   Ocean. The opposite spatial pattern and trend represented by node 7 is
   associated with a wave train originating over northern Australia. The
   anomalous wind field, surface downward longwave radiation, and surface
   air temperature generated by these circulation patterns are consistent
   with the spatial pattern and overall trends in the Antarctic sea ice
   cover.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Yu, LJ (Corresponding Author), Polar Res Inst China, State Ocean Adm Key Lab Polar Sci, Shanghai, Peoples R China.
   Yu, LJ (Corresponding Author), Michigan State Univ, Dept Geog Environm \& Spatial Sci, E Lansing, MI 48824 USA.
   Yu, Lejiang; Zhou, Mingyu; Sun, Bo, Polar Res Inst China, State Ocean Adm Key Lab Polar Sci, Shanghai, Peoples R China.
   Yu, Lejiang; Zhong, Shiyuan, Michigan State Univ, Dept Geog Environm \& Spatial Sci, E Lansing, MI 48824 USA.
   Zhou, Mingyu, Natl Marine Environm Predict Ctr, Beijing, Peoples R China.
   Lenschow, Donald H., Natl Ctr Atmospher Res, POB 3000, Boulder, CO 80307 USA.}},
DOI = {{10.1175/JCLI-D-17-0739.1}},
ISSN = {{0894-8755}},
EISSN = {{1520-0442}},
Keywords = {{Atmosphere-ocean interaction; Sea state; Climate change; Climate
   variability; Ice loss; growth}},
Keywords-Plus = {{SELF-ORGANIZING MAPS; SOUTHERN-OCEAN; LONG-TERM; CLIMATE; IMPACTS;
   TELECONNECTION; VARIABILITY; PERFORMANCE; EXTRACTION; EXPANSION}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{yulejiang@sina.com.cn}},
Funding-Acknowledgement = {{Shanghai Pujiang ProgramShanghai Pujiang Program {[}17PJ1409800]}},
Funding-Text = {{This study is sponsored by the Shanghai Pujiang Program (17PJ1409800).}},
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Number-of-Cited-References = {{44}},
Times-Cited = {{4}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{18}},
Journal-ISO = {{J. Clim.}},
Doc-Delivery-Number = {{GD5II}},
Unique-ID = {{ISI:000430540200008}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000430539000010,
Author = {Tolika, Konstantia and Maheras, Panagiotis and Anagnostopoulou,
   Christina},
Title = {{The exceptionally wet year of 2014 over Greece: a statistical and
   synoptical-atmospheric analysis over the region of Thessaloniki}},
Journal = {{THEORETICAL AND APPLIED CLIMATOLOGY}},
Year = {{2018}},
Volume = {{132}},
Number = {{3-4}},
Pages = {{809-821}},
Month = {{MAY}},
Abstract = {{The highest rainfall totals (912.2 mm) and the largest number of
   raindays (133 days), since 1958, were recorded in Thessaloniki during
   the year of 2014. Extreme precipitation heights were also observed on a
   seasonal, monthly and daily basis. The examined year presented the
   highest daily rainfall intensity, the maximum daily precipitation and
   the largest number of heavy precipitation days (greater than 10 mm), and
   it also exceeded the previous amounts of precipitation of very wet (95th
   percentile) and extremely wet (99th percentile) days. According to the
   automatic circulation type classification scheme that was used, it was
   found that during this exceptionally wet year, the frequency of
   occurrence of cyclonic types at the near surface geopotential level
   increases, while the same types decreased at a higher atmospheric level
   (500 hPa). The prevailing type was type C which is located at the centre
   of the study area (Greece), but several other cyclonic types changed
   during this year not only their frequency but also their percentage of
   rainfall as well as their daily precipitation intensity. It should be
   highlighted that these findings differentiated on the seasonal-scale
   analysis. Moreover, out of the three teleconnection patterns that were
   examined (Scandinavian Pattern, Eastern Mediterranean Teleconnection
   Pattern and North Sea-Caspian Pattern), the Scandinavian one (SCAND) was
   detected during the most of the months of 2014 meaning that it was
   highly associated with intense precipitation over Greece.}},
Publisher = {{SPRINGER WIEN}},
Address = {{SACHSENPLATZ 4-6, PO BOX 89, A-1201 WIEN, AUSTRIA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Tolika, K (Corresponding Author), Aristotle Univ Thessaloniki, Sch Geol, Dept Meteorol \& Climatol, Thessaloniki 55124, Greece.
   Tolika, Konstantia; Maheras, Panagiotis; Anagnostopoulou, Christina, Aristotle Univ Thessaloniki, Sch Geol, Dept Meteorol \& Climatol, Thessaloniki 55124, Greece.}},
DOI = {{10.1007/s00704-017-2131-8}},
ISSN = {{0177-798X}},
EISSN = {{1434-4483}},
Keywords-Plus = {{MEDITERRANEAN TELECONNECTION PATTERN; PRECIPITATION EXTREMES;
   CIRCULATION TYPES; CLIMATE EXTREMES; RAINFALL; CLASSIFICATION;
   TEMPERATURE; VARIABILITY; FREQUENCY; TRENDS}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{diatol@geo.auth.gr}},
ResearcherID-Numbers = {{Anagnostopoulou, Christina/M-3942-2019}},
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   Tolika K, 2007, ADV GEOSCI, V12, DOI DOI 10.5194/ADGE0-12-87-2007.
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Number-of-Cited-References = {{37}},
Times-Cited = {{4}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{0}},
Journal-ISO = {{Theor. Appl. Climatol.}},
Doc-Delivery-Number = {{GD5HW}},
Unique-ID = {{ISI:000430539000010}},
DA = {{2020-08-06}},
}

@article{ ISI:000430539000022,
Author = {Harris, Sarah M. and Carvalho, Leila M. V.},
Title = {{Characteristics of southern California atmospheric rivers}},
Journal = {{THEORETICAL AND APPLIED CLIMATOLOGY}},
Year = {{2018}},
Volume = {{132}},
Number = {{3-4}},
Pages = {{965-981}},
Month = {{MAY}},
Abstract = {{Atmospheric rivers (ARs) are channels of high water vapor flux that
   transport moisture from low to higher latitudes on synoptic timescales.
   In areas of topographical variability, ARs may lead to high-intensity
   precipitation due to orographic forcing. ARs landfalling along North
   America's west coast are linked to extreme events including those
   leading to flooding and landslides. In southern California (SCA), proper
   AR forecasting is important for regional water resources as well as
   hazard mitigation and as the area's annual precipitation totals occur
   from relatively few storms per season, any changes to storm frequency
   and/or intensity may have dramatic consequences. Yet, as most regional
   AR studies focus on the Pacific Northwest, there is little information
   about SCA ARs. We develop an algorithm to identify ARs landfalling on
   North America's west coast between 1979 and 2013 within total
   precipitable water reanalysis fields. ARs are then categorized according
   to landfall region. To determine and differentiate the characteristics
   and spatial distributions of ARs affecting these areas, we examine lag
   composites of various atmospheric variables for each landfall region.
   SCA ARs differ from ARs landfalling farther north in the days prior to
   landfall with the position and amplitude of a trough offshore from the
   Asian continent and ridge over Alaska, as well as the displacement and
   eastward extension of the jet core that potentially guides AR moisture
   southwards. The relationships between AR landfalls and the El
   Nio/Southern Oscillation (ENSO), the Madden-Julian Oscillation (MJO),
   and the Pacific/North American Teleconnection Pattern (PNA) are also
   investigated.}},
Publisher = {{SPRINGER WIEN}},
Address = {{SACHSENPLATZ 4-6, PO BOX 89, A-1201 WIEN, AUSTRIA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Harris, SM (Corresponding Author), Univ Calif Santa Barbara, Dept Geog, 1832 Ellison Hall, Santa Barbara, CA 93106 USA.
   Harris, Sarah M.; Carvalho, Leila M. V., Univ Calif Santa Barbara, Dept Geog, 1832 Ellison Hall, Santa Barbara, CA 93106 USA.
   Carvalho, Leila M. V., Earth Res Inst, Santa Barbara, CA USA.}},
DOI = {{10.1007/s00704-017-2138-1}},
ISSN = {{0177-798X}},
EISSN = {{1434-4483}},
Keywords-Plus = {{WESTERN UNITED-STATES; EXTREME PRECIPITATION; INLAND PENETRATION;
   PACIFIC-OCEAN; NORTH PACIFIC; MOISTURE; SATELLITE; OSCILLATION;
   CONNECTION; RAINFALL}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{sarah.harris@geog.ucsb.edu}},
Funding-Acknowledgement = {{University of California Graduate DivisionUniversity of California
   System}},
Funding-Text = {{The authors greatly appreciate many helpful discussions with Charles
   Jones who was crucial to the algorithm's development. The availability
   of CFSR data as well as ONI and PNA indices from NOAA was very helpful.
   Sarah M. Harris is grateful for financial support from the University of
   California Graduate Division.}},
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Number-of-Cited-References = {{41}},
Times-Cited = {{7}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{16}},
Journal-ISO = {{Theor. Appl. Climatol.}},
Doc-Delivery-Number = {{GD5HW}},
Unique-ID = {{ISI:000430539000022}},
DA = {{2020-08-06}},
}

@article{ ISI:000429529900009,
Author = {Zhang, Lixia and Wu, Peili and Zhou, Tianjun and Xiao, Chan},
Title = {{ENSO Transition from La Nina to El Nino Drives Prolonged Spring-Summer
   Drought over North China}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2018}},
Volume = {{31}},
Number = {{9}},
Pages = {{3509-3523}},
Month = {{MAY}},
Abstract = {{Persistent drought is a major meteorological disaster causing vast
   agricultural damage and long-term regional water crises. Over north
   China, this type of drought tends to begin in spring and to persist
   until summer with severe societal impacts. This paper aims to identify
   the large-scale dynamic drivers of the prolonged spring-summer drought
   (PSSD) over north China. This analysis has shown that the north China
   PSSD is associated with a persistent anomalous low-level cyclonic
   circulation spanning the midlatitude North Pacific from spring to summer
   with reduced moisture transport to north China, in combination with a
   tropospheric cooling along the East Asian upper-level westerly jet with
   dynamically forced anomalous descent above. Seven of the selected eight
   north China PSSD events occurred when La Nina transitioned to El Nino
   with a negative North Pacific Oscillation (NPO) phase in the preceding
   winter. The two key circulation anomalies in spring are set directly by
   a negative NPO phase generated in the preceding winter. The NPO, in
   turn, forces an El Nino onset in summer through the so-called seasonal
   footprinting mechanism. Consequently, sea surface temperature anomalies
   of El Nino in summer suppress Indian monsoon rainfall, triggering the
   tropospheric temperature cooling over East Asia through a circumglobal
   teleconnection along the East Asian upper-level westerly jet. Modeling
   analysis of the long preindustrial control simulation confirms the above
   findings. This study demonstrates that ENSO phase transition from La
   Nina to El Nino is one of the important precursors of north China PSSD.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Zhang, LX (Corresponding Author), Chinese Acad Sci, Inst Atmospher Phys, LASG, Beijing, Peoples R China.
   Zhang, LX (Corresponding Author), Nanjing Univ Informat Sci \& Technol, Collaborat Innovat Ctr Forecast \& Evaluat Meteoro, Nanjing, Jiangsu, Peoples R China.
   Zhang, Lixia, Chinese Acad Sci, Inst Atmospher Phys, LASG, Beijing, Peoples R China.
   Zhang, Lixia, Nanjing Univ Informat Sci \& Technol, Collaborat Innovat Ctr Forecast \& Evaluat Meteoro, Nanjing, Jiangsu, Peoples R China.
   Wu, Peili, Met Off Hadley Ctr, Exeter, Devon, England.
   Zhou, Tianjun, Inst Atmospher Phys, LASG, Beijing, Peoples R China.
   Zhou, Tianjun, Univ Chinese Acad Sci, Chinese Acad Sci, Beijing, Peoples R China.
   Xiao, Chan, China Meteorol Adm, Natl Climate Ctr, Beijing, Peoples R China.}},
DOI = {{10.1175/JCLI-D-17-0440.1}},
ISSN = {{0894-8755}},
EISSN = {{1520-0442}},
Keywords-Plus = {{SEASONAL FOOTPRINTING MECHANISM; INTERANNUAL VARIABILITY; INDIAN-OCEAN;
   EAST-ASIA; PACIFIC; MONSOON; TELECONNECTION; PRECIPITATION; ANOMALIES;
   CLIMATE}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{lixiazhang@mail.iap.ac.cn}},
ResearcherID-Numbers = {{ZHOU, Tianjun/C-3195-2012}},
ORCID-Numbers = {{ZHOU, Tianjun/0000-0002-5829-7279}},
Funding-Acknowledgement = {{National Natural Science Foundation of ChinaNational Natural Science
   Foundation of China {[}41675076, 41661144009]; Program of International
   ST Cooperation {[}2016YFE0102400]; U.K.-China Research and Innovation
   Partnership Fund through the Met Office Climate Science for Service
   Partnership (CSSP) China as part of the Newton Fund}},
Funding-Text = {{This work was jointly supported by the National Natural Science
   Foundation of China under Grants 41675076 and 41661144009 and Program of
   International S\&T Cooperation under Grant 2016YFE0102400. Met Office
   staff is supported by the U.K.-China Research and Innovation Partnership
   Fund through the Met Office Climate Science for Service Partnership
   (CSSP) China as part of the Newton Fund.}},
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Number-of-Cited-References = {{57}},
Times-Cited = {{5}},
Usage-Count-Last-180-days = {{2}},
Usage-Count-Since-2013 = {{38}},
Journal-ISO = {{J. Clim.}},
Doc-Delivery-Number = {{GC1GW}},
Unique-ID = {{ISI:000429529900009}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000429529900010,
Author = {He, Zhuoqi and Wu, Renguang},
Title = {{Change in Coherence of Interannual Variability of Summer Rainfall over
   the Western Pacific around the Early 2000s: Role of Indo-Pacific Ocean
   Forcing}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2018}},
Volume = {{31}},
Number = {{9}},
Pages = {{3525-3538}},
Month = {{MAY}},
Abstract = {{The observations show that the covariability between the western North
   Pacific (WNP) and the South China Sea (SCS) summer rainfall has
   experienced an obvious weakening since the early 2000s. During the
   period 1982-2003, the combined north Indian Ocean (NIO), central North
   Pacific (CNP), and central equatorial Pacific (CEP) sea surface
   temperature (SST) forcing results in a high coherence between the WNP
   and SCS summer rainfall variations via a zonally elongated anomalous
   lower-level cyclone over the western Pacific. During the period 2004-16,
   the Indian Ocean SST contribution is largely weakened, and the WNP
   rainfall variability is dominated by the enhanced Pacific SST forcing
   with an eastward retreated lower-level wind and rainfall anomalies,
   whereas the SCS rainfall variability is mainly associated with local
   air-sea interaction processes. The results obtained from observational
   analysis are supported by numerical experiments with atmospheric and
   coupled general circulation models. The change in the coherence of
   interannual summer rainfall variability over the WNP and SCS has
   important implications for regional climate prediction in South and East
   Asia.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{He, ZQ (Corresponding Author), Chinese Acad Sci, South China Sea Inst Oceanol, State Key Lab Trop Oceanog, Guangzhou, Guangdong, Peoples R China.
   He, ZQ (Corresponding Author), Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci \& Geop, Beijing, Peoples R China.
   He, Zhuoqi, Chinese Acad Sci, South China Sea Inst Oceanol, State Key Lab Trop Oceanog, Guangzhou, Guangdong, Peoples R China.
   He, Zhuoqi; Wu, Renguang, Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci \& Geop, Beijing, Peoples R China.
   Wu, Renguang, Chinese Acad Sci, Ctr Monsoon Syst Res, Beijing, Peoples R China.}},
DOI = {{10.1175/JCLI-D-17-0687.1}},
ISSN = {{0894-8755}},
EISSN = {{1520-0442}},
Keywords-Plus = {{EAST ASIAN TELECONNECTION; AIR-SEA INTERACTION; EL-NINO; INDIAN-OCEAN;
   NORTH PACIFIC; MONSOON}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{zhuoqi@scsio.ac.cn}},
Funding-Acknowledgement = {{National Key Basic Research Program of ChinaNational Basic Research
   Program of China {[}2014CB953902]; National Natural Science Foundation
   of ChinaNational Natural Science Foundation of China {[}41506003,
   41530425, 41676013, 41731173, 41776023]; Independent Research Project
   Program of State Key Laboratory of Tropical Oceanography {[}LTOZZ1603]}},
Funding-Text = {{This study is supported by the National Key Basic Research Program of
   China (Grant 2014CB953902), the National Natural Science Foundation of
   China (Grants 41506003, 41530425, 41676013, 41731173, and 41776023), and
   the Independent Research Project Program of State Key Laboratory of
   Tropical Oceanography (LTOZZ1603). The NOAA IO v2 SST, GPCP version 2.2
   precipitation, NCEP-DOE Reanalysis 2, and NCEP GODAS data are obtained
   from http://www.esrl.noaa.gov/psd/data.}},
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Number-of-Cited-References = {{35}},
Times-Cited = {{4}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{5}},
Journal-ISO = {{J. Clim.}},
Doc-Delivery-Number = {{GC1GW}},
Unique-ID = {{ISI:000429529900010}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000429650700002,
Author = {Barrett, Hannah G. and Jones, Julie M. and Bigg, Grant R.},
Title = {{Reconstructing El Nino Southern Oscillation using data from ships'
   logbooks, 1815-1854. Part II: Comparisons with existing ENSO
   reconstructions and implications for reconstructing ENSO diversity}},
Journal = {{CLIMATE DYNAMICS}},
Year = {{2018}},
Volume = {{50}},
Number = {{9-10}},
Pages = {{3131-3152}},
Month = {{MAY}},
Abstract = {{A systematic comparison of El Nino Southern Oscillation reconstructions
   during the early to mid-nineteenth century is presented using a range of
   proxy and documentary sources. Reconstructions of the boreal winter
   Southern Oscillation Index (SOI) using data from ships' logbooks
   presented in a companion paper are evaluated and compared to previous
   ENSO reconstructions. Comparisons between ENSO reconstructions and the
   instrumental SOI during a period of overlap (1876-1977) are made. These
   same proxy and documentary reconstructions are then compared to the
   logbook-based reconstructions, over 1815-1854. The logbook-based
   reconstructions compare best with a recent multi-proxy reconstruction
   that used signals taken from different teleconnection regions, and they
   have an improved agreement with multi-proxy records compared to a
   previous attempt to reconstruct the SOI from ships' logbook data. The
   logbook-based and the multi-proxy reconstructions are found to capture
   El Nino events better than La Nina events, and East Pacific El Nino
   events better than Central Pacific El Nino events, thus suggesting a
   degree of bias in the historical reconstructions. These findings have
   important implications for future ENSO reconstructions, with a need for
   an increased understanding of the effects of different ENSO flavours for
   future reconstructions.}},
Publisher = {{SPRINGER}},
Address = {{233 SPRING ST, NEW YORK, NY 10013 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Barrett, HG (Corresponding Author), Univ Sheffield, Dept Geog, Winter St, Sheffield S10 2TN, S Yorkshire, England.
   Barrett, Hannah G.; Jones, Julie M.; Bigg, Grant R., Univ Sheffield, Dept Geog, Winter St, Sheffield S10 2TN, S Yorkshire, England.}},
DOI = {{10.1007/s00382-017-3797-4}},
ISSN = {{0930-7575}},
EISSN = {{1432-0894}},
Keywords = {{ENSO reconstruction; Climate variability; Ships' logbooks; Multi-proxy
   comparison; ENSO flavours}},
Keywords-Plus = {{TEMPERATURE; EVENTS; PROXY; VARIABILITY; RAINFALL; PACIFIC; FLAVORS;
   INDEX}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{hannahgbarrett@hotmail.com}},
ORCID-Numbers = {{Jones, Julie/0000-0003-2892-8647}},
Funding-Acknowledgement = {{Department of Geography at the University of Sheffield}},
Funding-Text = {{We thank the Department of Geography at the University of Sheffield for
   supporting this research.}},
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Number-of-Cited-References = {{53}},
Times-Cited = {{2}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{4}},
Journal-ISO = {{Clim. Dyn.}},
Doc-Delivery-Number = {{GC2YM}},
Unique-ID = {{ISI:000429650700002}},
OA = {{Green Accepted, Other Gold}},
DA = {{2020-08-06}},
}

@article{ ISI:000428973000011,
Author = {Hong, Bing and Uchida, Masao and Hong, Yetang and Peng, Haijun and
   Kondo, Miyuki and Ding, Hanwei},
Title = {{The respective characteristics of millennial-scale changes of the India
   summer monsoon in the Holocene and the Last Glacial}},
Journal = {{PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY}},
Year = {{2018}},
Volume = {{496}},
Pages = {{155-165}},
Month = {{MAY 1}},
Abstract = {{There has been no proxy climate record simultaneously showing the
   identified millennial-scale change events of the India summer monsoon
   (ISM) during the period from the Last Glacial period to the Holocene,
   although these abrupt changes have been shown in separate records. This
   deficiency prevents further understanding of the potentially different
   characteristics of the ISM rapid changes. Here, we present a 33,300-year
   record of the ISM reconstructed from the stable carbon isotopic
   composition of cellulose in peat deposits collected near the Tibetan
   Plateau, reflecting the millennial-scale history of abrupt changes in
   the ISM intensity from the cold late Last Glacial to the warm Holocene
   epoch. Our record shows that, corresponding to the abrupt cooling
   (warming) events that occur in the high northern latitudes, the ISM
   intensity abruptly decreases (increases), which provides additional
   evidence for the teleconnection between low-latitude monsoonal
   variability and the rapid temperature fluctuation of high northern
   latitudes. However, this relationship behaves differently in the cold
   and warm stages. In the cold late Last Glacial period, a one-to-one
   response is often seen, but in the warm Holocene, the ISM often shows
   only partial responses to the rapid cooling events. In particular, more
   than half of the abruptly weakening events in the ISM occur in the
   Holocene, and the amplitudes of declines are larger in the warm stage
   than in the cold stage, which reveals that extreme change events in the
   ISM have occurred much more in the warm Holocene and may have once
   influenced the development of ancient civilizations. We consider that
   the various characteristics of the abrupt changes in the ISM during the
   warm and cold stages may have derived from different combinations of
   climatic drivers within the two stages. These results provide a
   historical record of the considerable changes in ISM and resultant
   effects on human society, and so provide a background for concerns over
   contemporary climate change.}},
Publisher = {{ELSEVIER SCIENCE BV}},
Address = {{PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Hong, YT (Corresponding Author), Chinese Acad Sci, Inst Geochem, State Key Lab Environm Geochem, 99 Lincheng Rd West, Guiyang 550081, Guizhou, Peoples R China.
   Hong, Bing; Hong, Yetang; Peng, Haijun; Ding, Hanwei, Chinese Acad Sci, Inst Geochem, State Key Lab Environm Geochem, 99 Lincheng Rd West, Guiyang 550081, Guizhou, Peoples R China.
   Uchida, Masao; Kondo, Miyuki, Natl Inst Environm Studies, Ctr Environm Measurement \& Anal, Onogawa 16-2, Tsukuba, Ibaraki 3050053, Japan.}},
DOI = {{10.1016/j.palaeo.2018.01.033}},
ISSN = {{0031-0182}},
EISSN = {{1872-616X}},
Keywords = {{Extreme climate event; Abrupt climate change; Global warming; Bond
   event; Peat}},
Keywords-Plus = {{NORTH-ATLANTIC CLIMATE; ASIAN MONSOON; HIGH-RESOLUTION; ICE-CORE;
   ARABIAN SEA; OCEAN CIRCULATION; HEINRICH EVENTS; PEAT CELLULOSE;
   TIME-SERIES; DEEP-SEA}},
Research-Areas = {{Physical Geography; Geology; Paleontology}},
Web-of-Science-Categories  = {{Geography, Physical; Geosciences, Multidisciplinary; Paleontology}},
Author-Email = {{hongyetang@vip.skleg.cn}},
ResearcherID-Numbers = {{Peng, Haijun/AAV-2687-2020
   }},
ORCID-Numbers = {{Peng, Haijun/0000-0002-2341-3882}},
Funding-Acknowledgement = {{National Natural Science Foundation of ChinaNational Natural Science
   Foundation of China {[}41373134, 41173127, 41773140]}},
Funding-Text = {{This work was supported by the National Natural Science Foundation of
   China (Grant Nos. 41373134, 41173127, 41773140).}},
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Number-of-Cited-References = {{99}},
Times-Cited = {{4}},
Usage-Count-Last-180-days = {{2}},
Usage-Count-Since-2013 = {{19}},
Journal-ISO = {{Paleogeogr. Paleoclimatol. Paleoecol.}},
Doc-Delivery-Number = {{GB3QR}},
Unique-ID = {{ISI:000428973000011}},
DA = {{2020-08-06}},
}

@article{ ISI:000428973200035,
Author = {Ajtic, J. and Brattich, E. and Sarvan, D. and Djurdjevic, V. and
   Hernandez-Ceballos, M. A.},
Title = {{Factors affecting the Be-7 surface concentration and its extremely high
   occurrences over the Scandinavian Peninsula during autumn and winter}},
Journal = {{CHEMOSPHERE}},
Year = {{2018}},
Volume = {{199}},
Pages = {{278-285}},
Month = {{MAY}},
Abstract = {{Relationships between the beryllium-7 activity concentrations in surface
   air and meteorological parameters (temperature, atmospheric pressure,
   and precipitation), teleconnection indices (Arctic Oscillation, North
   Atlantic Oscillation, and Scandinavian pattern) and number of sunspots
   are investigated using two multivariate statistical techniques:
   hierarchical cluster and factor analysis. The beryllium-7 surface
   measurements over 1995-2011, at four sampling sites located in the
   Scandinavian Peninsula, are obtained from the Radioactivity
   Environmental Monitoring Database. In all sites, the statistical
   analyses show that the beryllium-7 concentrations are strongly linked to
   temperature. Although the beryllium-7 surface concentration exhibits the
   well-characterised spring/summer maximum, our study shows that extremely
   high beryllium-7 concentrations, defined as the values exceeding the
   90th percentile in the data records for each site, also occur over the
   October-March period. Two types of autumn/winter extremes are
   distinguished: type-1 when the number of extremes in a given month is
   less than three, and type-2 when at least three extremes occur in a
   month. Factor analysis performed for these autumn/winter events shows a
   weaker effect of temperature and a stronger impact of the transport and
   production signal on the beryllium-7 concentrations. Further, the
   majority of the type-2 extremes are associated with a very high monthly
   Scandinavian teleconnection index. The type-2 extremes that occurred in
   January, February and March are also linked to sudden stratospheric
   warmings of the Arctic vortex. Our results indicate that the
   Scandinavian teleconnection index might be a good indicator of the
   meteorological conditions facilitating extremely high beryllium-7
   surface concentrations over Scandinavia during autumn and winter. (C)
   2018 Elsevier Ltd. All rights reserved.}},
Publisher = {{PERGAMON-ELSEVIER SCIENCE LTD}},
Address = {{THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Ajtic, J (Corresponding Author), Univ Belgrade, Fac Vet Med, Bulevar Oslobodenja 18, Belgrade 11000, Serbia.
   Ajtic, J.; Sarvan, D., Univ Belgrade, Fac Vet Med, Bulevar Oslobodenja 18, Belgrade 11000, Serbia.
   Brattich, E., Alma Mater Studiorum Univ Bologna, Dept Phys \& Astron, Via Irnerio 46, I-40126 Bologna, BO, Italy.
   Djurdjevic, V., Univ Belgrade, Inst Meteorol, Fac Phys, Studentski Trg 18, Belgrade 11000, Serbia.
   Hernandez-Ceballos, M. A., European Commiss, Joint Res Ctr, Knowledge Nucl Secur \& Safety Unit, Radioact Environm Monitoring Grp, Via Enrico Fermi 2749, I-21027 Ispra, VA, Italy.}},
DOI = {{10.1016/j.chemosphere.2018.02.052}},
ISSN = {{0045-6535}},
EISSN = {{1879-1298}},
Keywords = {{Beryllium-7; Surface air; Meteorological parameters; Teleconnection
   indices; Multivariate analysis; Sudden stratospheric warming}},
Keywords-Plus = {{TROPOPAUSE HEIGHT; COSMOGENIC BE-7; AIR; BERYLLIUM-7; TRANSPORT;
   RADIONUCLIDES; PB-210; STRATOSPHERE; CLIMATOLOGY; VARIABILITY}},
Research-Areas = {{Environmental Sciences \& Ecology}},
Web-of-Science-Categories  = {{Environmental Sciences}},
Author-Email = {{jelena.ajtic@vet.bg.ac.rs
   erika.brattich@unibo.it
   darko.sarvan@vet.bg.ac.rs
   vdj@ff.bg.ac.rs
   miguel-angel.hernandez-ceballos@ec.europa.eu}},
ResearcherID-Numbers = {{Brattich, Erika/D-5127-2018}},
ORCID-Numbers = {{Brattich, Erika/0000-0001-8402-7611}},
Funding-Acknowledgement = {{Ministry of Education, Science and Technological Development of the
   Republic of Serbia {[}43007]}},
Funding-Text = {{The paper is a part of the research done within the project ``Climate
   changes and their influence on the environment: impacts, adaptation and
   mitigation{''} (No. 43007) financed by the Ministry of Education,
   Science and Technological Development of the Republic of Serbia
   (2011-2018). The authors would like to thank the REM group for the
   provision of the <SUP>7</SUP>Be activity concentration measurements from
   the REM database (REMdb, REM group of the DG Joint Research Centre,
   Ispra site, European Commission) and the EU Member States for providing
   the <SUP>7</SUP>Be data. Erika Brattich is especially grateful to Prof.
   Laura Tositti for what she taught her during her Ph.D. and post-doctoral
   studies.}},
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