text:
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Number-of-Cited-References = {{46}},
Times-Cited = {{1}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{2}},
Journal-ISO = {{Tellus Ser. A-Dyn. Meteorol. Oceanol.}},
Doc-Delivery-Number = {{728YF}},
Unique-ID = {{ISI:000185743400003}},
DA = {{2020-08-06}},
}

@article{ ISI:000185699500011,
Author = {Tamburini, F and Adatte, T and Follmi, K and Bernasconi, SM and
   Steinmann, P},
Title = {{Investigating the history of East Asian monsoon and climate during the
   last glacial-interglacial period (0-140 000 years): mineralogy and
   geochemistry of ODP Sites 1143 and 1144, South China Sea}},
Journal = {{MARINE GEOLOGY}},
Year = {{2003}},
Volume = {{201}},
Number = {{1-3}},
Pages = {{147-168}},
Month = {{SEP 30}},
Note = {{Symposium on Asian Monsoons and Global Linkages on Milankovitch and
   Sub-Milankovitch Time Scales, BEIJING, PEOPLES R CHINA, MAY 09-11, 2001}},
Abstract = {{Monsoon climate is an important component of the global climatic system.
   A comprehensive understanding of its variability over
   glacial-interglacial time scales as well as of its effects on the
   continent and in the ocean is required to decipher links between
   climate, continental weathering and productivity. A detailed multiproxy
   study, including bulk and clay mineralogy, grain-size analysis,
   phosphorus geochemistry (SEDEX extraction), organic matter
   characterization, and nitrogen stable isotopes, was carried out on
   samples from ODP Sites 1143 and 1144 (Leg 184, South China Sea),
   covering the past 140 000 years. We tentatively reconstruct the complex
   sedimentation and climatic history of the region during the last
   glacial-interglacial cycle, when sea-level variations, linked to the
   growth and melting of ice caps, interact with monsoon variability.
   During interglacial periods of high sea level, summer monsoon was
   strong, and humid and warm climate characterized the adjacent continent
   and islands. Clay minerals bear signals of chemical weathering during
   these intervals. High calcite and reactive phosphorus mass accumulation
   rates (MARs) indicate high productivity, especially in the southern
   region of the basin. During glacial intervals, strong winter monsoon
   provided enhanced detrital input from the continent, as indicated by
   high detrital MAR. Glacial low sea level resulted in erosion of
   sediments from the exposed Sunda shelf to the south, and clay mineral
   variations indicate that warm and humid conditions still prevailed in
   the southern tropical areas. Enhanced supply of nutrients from the
   continent, both by river and eolian input, maintained high primary
   productivity. Reduced circulation during these periods possibly induced
   active remobilization of nutrients, such as phosphorus, from the
   sediments. Intense and short cold periods recorded during glacial and
   interglacial stages correlate with loess records in China and marine
   climatic records in the North Atlantic, confirming a teleconnection
   between low- and high-latitude climate variability. (C) 2003 Elsevier
   B.V. All rights reserved.}},
Publisher = {{ELSEVIER SCIENCE BV}},
Address = {{PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS}},
Type = {{Article; Proceedings Paper}},
Language = {{English}},
Affiliation = {{Tamburini, F (Corresponding Author), ETH Zentrum, Inst Geol, CH-8092 Zurich, Switzerland.
   ETH Zentrum, Inst Geol, CH-8092 Zurich, Switzerland.
   Univ Neuchatel, Inst Geol, CH-2007 Neuchatel, Switzerland.}},
DOI = {{10.1016/S0025-3227(03)00214-7}},
ISSN = {{0025-3227}},
Keywords = {{South China Sea; Pleistocene-Holocene climate; monsoon; continent-ocean
   interaction; phosphorus geochemistry}},
Keywords-Plus = {{ROCK-EVAL PYROLYSIS; OXYGEN MINIMUM ZONE; MARINE-SEDIMENTS;
   ORGANIC-MATTER; ARABIAN SEA; PHOSPHORUS REGENERATION; SEQUENTIAL
   EXTRACTION; ISOTOPIC COMPOSITION; NUTRIENT UTILIZATION; NORTH-ATLANTIC}},
Research-Areas = {{Geology; Oceanography}},
Web-of-Science-Categories  = {{Geosciences, Multidisciplinary; Oceanography}},
ResearcherID-Numbers = {{Bernasconi, Stefano M/E-5394-2010
   }},
ORCID-Numbers = {{Bernasconi, Stefano M/0000-0001-7672-8856
   Tamburini, Federica/0000-0001-6871-1915}},
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Number-of-Cited-References = {{62}},
Times-Cited = {{97}},
Usage-Count-Last-180-days = {{7}},
Usage-Count-Since-2013 = {{35}},
Journal-ISO = {{Mar. Geol.}},
Doc-Delivery-Number = {{728DG}},
Unique-ID = {{ISI:000185699500011}},
DA = {{2020-08-06}},
}

@article{ ISI:000185476800001,
Author = {Kodera, K and Kuroda, Y},
Title = {{Regional and hemispheric circulation patterns in the northern hemisphere
   winter, or the NAO and the AO}},
Journal = {{GEOPHYSICAL RESEARCH LETTERS}},
Year = {{2003}},
Volume = {{30}},
Number = {{18}},
Month = {{SEP 20}},
Abstract = {{{[} 1] Two different scales of teleconnection patterns are found over
   the Euro- Atlantic region during the winter. One is a regional seesaw
   between Iceland and the Azores, and the other is a hemispheric seesaw
   between the Mediterranean and the polar- Siberia region. The North
   Atlantic Oscillation ( NAO) and the Arctic Oscillation ( AO) indices are
   sensitive to both modes, although the NAO index reflects the more
   regional one. The principal process producing a hemispheric seesaw
   pattern in the surface pressure is changing in vertical winds in the
   polar troposphere driven by wave forcings. Upward motion in the polar
   region induces meridional flows near the surface, especially around the
   Norwegian Sea and Bering Strait, which induce wavy patterns in the
   surface pressure. The importance of distinguishing the two modes in
   understanding recent trends is also addressed.}},
Publisher = {{AMER GEOPHYSICAL UNION}},
Address = {{2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Kodera, K (Corresponding Author), Meteorol Res Inst, 1-1 Nagamine, Tsukuba, Ibaraki 3050052, Japan.
   Meteorol Res Inst, Tsukuba, Ibaraki 3050052, Japan.}},
DOI = {{10.1029/2003GL017290}},
Article-Number = {{1934}},
ISSN = {{0094-8276}},
EISSN = {{1944-8007}},
Keywords-Plus = {{APPARENT ARCTIC OSCILLATION; ATLANTIC OSCILLATION; SPATIAL STRUCTURE;
   ANNULAR MODE; VARIABILITY; TELECONNECTIONS; EUROPE; TRUE}},
Research-Areas = {{Geology}},
Web-of-Science-Categories  = {{Geosciences, Multidisciplinary}},
Author-Email = {{kodera@mri-jma.go.jp
   kuroda@mri-jma.go.jp}},
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Number-of-Cited-References = {{17}},
Times-Cited = {{18}},
Usage-Count-Last-180-days = {{4}},
Usage-Count-Since-2013 = {{9}},
Journal-ISO = {{Geophys. Res. Lett.}},
Doc-Delivery-Number = {{724FD}},
Unique-ID = {{ISI:000185476800001}},
DA = {{2020-08-06}},
}

@article{ ISI:000185670500012,
Author = {Xue, F and Jiang, DB and Lang, XM and Wang, HJ},
Title = {{Influence of the mascarene high and Australian high on the summer
   monsoon in East Asia: Ensemble simulation}},
Journal = {{ADVANCES IN ATMOSPHERIC SCIENCES}},
Year = {{2003}},
Volume = {{20}},
Number = {{5}},
Pages = {{799-809}},
Month = {{SEP}},
Abstract = {{By using a nine-level atmospheric general circulation model developed at
   the Institute of Atmospheric Physics (IAP 9L AGCM), two sets of
   numerical experiments are carried out to investigate the influence of
   the Mascarene high (MH) and Australian high (AH) over the southern
   subtropics upon the East Asian summer monsoon circulation and summer
   precipitation in East Asia. The use of ensemble statistics is adopted to
   reduce the simulation errors. The result shows that with the
   intensification of MH, the Somali low-level jet is significantly
   enhanced together with the summer monsoon circulation in the tropical
   Asia and western Pacific region. Furthermore, the anticyclonic anomaly
   in the tropical western Pacific to the east of the Philippines may
   induce a weak East-Asia-Pacific teleconnection pattern. In the meantime,
   geopotential height in the Tropics is enhanced while it is reduced over
   most regions of mid-high latitudes, thus the northwestern Pacific
   subtropical high at 500 hPa extends southwestward, resulting in more
   rainfall in southern China and less rainfall in northern China. A
   similar anomaly pattern of the atmospheric circulation systems is found
   in the experiment of the intensification of AH. On the other hand,
   because the cross-equatorial currents associated with AH are much weaker
   than the Somali jet, the anomaly magnitude caused by the intensification
   of AH is generally weak, and the influence of AH on summer rainfall in
   China seems to be localized in southern China. Comparison between the
   two sets of experiments indicates that MH plays a crucial role in the
   interactions of general atmospheric circulation between the two
   hemispheres.}},
Publisher = {{SCIENCE CHINA PRESS}},
Address = {{16 DONGHUANGCHENGGEN NORTH ST, BEIJING 100717, PEOPLES R CHINA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Xue, F (Corresponding Author), Acad Sinica, Inst Atmospher Phys, LASG, Beijing 100029, Peoples R China.
   Acad Sinica, Inst Atmospher Phys, LASG, Beijing 100029, Peoples R China.}},
ISSN = {{0256-1530}},
Keywords = {{mascarene high; Australian high; East Asian summer monsoon}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
ResearcherID-Numbers = {{Jiang, Dabang/I-2243-2014}},
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Number-of-Cited-References = {{23}},
Times-Cited = {{21}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{11}},
Journal-ISO = {{Adv. Atmos. Sci.}},
Doc-Delivery-Number = {{727QT}},
Unique-ID = {{ISI:000185670500012}},
DA = {{2020-08-06}},
}

@article{ ISI:000185228700002,
Author = {Krishnan, R and Sugi, M},
Title = {{Pacific decadal oscillation and variability of the Indian summer monsoon
   rainfall}},
Journal = {{CLIMATE DYNAMICS}},
Year = {{2003}},
Volume = {{21}},
Number = {{3-4}},
Pages = {{233-242}},
Month = {{SEP}},
Abstract = {{Recent studies have furnished evidence for interdecadal variability in
   the tropical Pacific Ocean. The importance of this phenomenon in causing
   persistent anomalies over different regions of the globe has drawn
   considerable attention in view of its relevance in climate assessment.
   Here, we examine multi-source climate records in order to identify
   possible signatures of this longer time scale variability on the Indian
   summer monsoon. The findings indicate a coherent inverse relationship
   between the inter-decadal fluctuations of Pacific Ocean sea surface
   temperature (SST) and the Indian monsoon rainfall during the last
   century. A warm (cold) phase of the Pacific interdecadal variability is
   characterized by a decrease (increase) in the monsoon rainfall and a
   corresponding increase (decrease) in the surface air temperature over
   the Indian subcontinent. This interdecadal relationship can also be
   confirmed from the teleconnection patterns evident from long-period sea
   level pressure (SLP) dataset. The SLP anomalies over South and Southeast
   Asia and the equatorial west Pacific are dynamically consistent in
   showing an out-of-phase pattern with the SLP anomalies over the tropical
   central-eastern Pacific. The remote influence of the Pacific
   interdecadal variability on the monsoon is shown to be associated with
   prominent signals in the tropical and southern Indian Ocean indicative
   of coherent inter-basin variability on decadal time scales. If indeed,
   the atmosphere-ocean coupling associated with the Pacific interdecadal
   variability is independent from that of the interannual El Nino-Southern
   Oscillation (ENSO), then the climate response should depend on the
   evolutionary characteristics of both the time scales. It is seen from
   our analysis that the Indian monsoon is more vulnerable to drought
   situations, when El Nino events occur during warm phases of the Pacific
   interdecadal variability. Conversely, wet monsoons are more likely to
   prevail, when La Nina events coincide during cold phases of the Pacific
   interdecadal variability.}},
Publisher = {{SPRINGER}},
Address = {{233 SPRING ST, NEW YORK, NY 10013 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Krishnan, R (Corresponding Author), Indian Inst Trop Meteorol, Dr Homi Bhabha Rd,NCL Post, Pune 411008, Maharashtra, India.
   Indian Inst Trop Meteorol, Pune 411008, Maharashtra, India.
   Meteorol Res Inst, Tsukuba, Ibaraki 305, Japan.
   FRSGC, Tsukuba, Ibaraki, Japan.}},
DOI = {{10.1007/s00382-003-0330-8}},
ISSN = {{0930-7575}},
Keywords-Plus = {{SEA-SURFACE TEMPERATURE; SOUTHERN OSCILLATION; CLIMATE VARIABILITY;
   NORTH PACIFIC; EL-NINO; INTERDECADAL CHANGES; ENSO; OCEAN; MODULATION;
   SYSTEM}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{krish@tropmet.res.in}},
ResearcherID-Numbers = {{sugi, masato/P-9076-2014}},
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Number-of-Cited-References = {{44}},
Times-Cited = {{133}},
Usage-Count-Last-180-days = {{2}},
Usage-Count-Since-2013 = {{25}},
Journal-ISO = {{Clim. Dyn.}},
Doc-Delivery-Number = {{719WU}},
Unique-ID = {{ISI:000185228700002}},
DA = {{2020-08-06}},
}

@article{ ISI:000185320000011,
Author = {Schimmelmann, A and Lange, CB and Meggers, BJ},
Title = {{Palaeoclimatic and archaeological evidence for a similar to 200-yr
   recurrence of floods and droughts linking California, Mesoamerica and
   South America over the past 2000 years}},
Journal = {{HOLOCENE}},
Year = {{2003}},
Volume = {{13}},
Number = {{5}},
Pages = {{763-778}},
Month = {{SEP}},
Abstract = {{Conspicuous grey, clay-rich flood deposits in the predominantly olive,
   varved sediment in the central Santa Barbara Basin, California, were
   dated via varve-counting to c. AD 212, 440, 603, 1029, 1418 and 1605.
   The similar to 200-yr quasi-periodicity and the timing of individual
   floods match time periods of known supraregional climatic changes and
   the documented similar to200-yr periodicity in palaeoclimate records
   elsewhere. The floods of c. ad 440 and ad 1418 occurred during global
   reorganizations of atmospheric circulation. Cold spells seem to have
   accompanied the floods of c. AD 1029 and ad 1605. California floods and
   other palaeoclimate records suggest that expressions of regional
   climates are modulated by solar variability with a similar to 200-yr
   periodicity. Our compilation of palaeoclimatic and Mesoamerican and
   South American archaeological records provides evidence that
   palaeoenvironmental and cultural changes were often coincident within
   their respective dating uncertainties and occurred in similar to 200-yr
   steps. The matching pattern supports the hypothesis that manifestations
   of changing climates, such as drought or flooding, served as
   destabilizing cofactors in transitions of precolumbian cultures.
   Extrapolation of the similar to 200-yr recurrence pattern of Santa
   Barbara flooding suggests that catastrophic flooding in southern
   California may be expected for the early part of this century.}},
Publisher = {{SAGE PUBLICATIONS LTD}},
Address = {{1 OLIVERS YARD, 55 CITY ROAD, LONDON EC1Y 1SP, ENGLAND}},
Type = {{Review}},
Language = {{English}},
Affiliation = {{Schimmelmann, A (Corresponding Author), Indiana Univ, Dept Geol Sci, 1001 E 10th St, Bloomington, IN 47405 USA.
   Indiana Univ, Dept Geol Sci, Bloomington, IN 47405 USA.
   Univ Concepcion, Dept Oceanog, Ctr Invest Oceanog Pacifico SurOriental, FONDAP, Concepcion 3, Chile.
   Smithsonian Inst, Washington, DC 20013 USA.}},
DOI = {{10.1191/0959683603hl661rp}},
ISSN = {{0959-6836}},
EISSN = {{1477-0911}},
Keywords = {{flood; drought; climatic change; solar variability; periodicity;
   teleconnection; cultural transition; Holocene; Santa Barbara Basin;
   California; Mesoamerica; South America}},
Keywords-Plus = {{STABLE-ISOTOPE RECORD; LATE-HOLOCENE CLIMATE; SAN-FRANCISCO BAY;
   TREE-RING WIDTH; ICE-AGE; EL-NINO; ATMOSPHERIC CIRCULATION;
   ENVIRONMENTAL-CHANGE; EXPLOSIVE VOLCANISM; SUMMER TEMPERATURES}},
Research-Areas = {{Physical Geography; Geology}},
Web-of-Science-Categories  = {{Geography, Physical; Geosciences, Multidisciplinary}},
Author-Email = {{aschimme@indiana.edu}},
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Number-of-Cited-References = {{152}},
Times-Cited = {{55}},
Usage-Count-Last-180-days = {{3}},
Usage-Count-Since-2013 = {{30}},
Journal-ISO = {{Holocene}},
Doc-Delivery-Number = {{721MK}},
Unique-ID = {{ISI:000185320000011}},
DA = {{2020-08-06}},
}

@article{ ISI:000185360600002,
Author = {Knippertz, P and Ulbrich, U and Marques, F and Corte-Real, J},
Title = {{Decadal changes in the link between El Nino and springtime North
   Atlantic oscillation and European-North African rainfall}},
Journal = {{INTERNATIONAL JOURNAL OF CLIMATOLOGY}},
Year = {{2003}},
Volume = {{23}},
Number = {{11}},
Pages = {{1293-1311}},
Month = {{SEP}},
Abstract = {{The link between El Nino-southern oscillation (ENSO) variability in
   boreal winter (represented by the NINO3 index, i.e. East Pacific
   sea-surface temperature anomalies) and the large-scale circulation and
   weather conditions over Europe-northwest Africa in spring is explored,
   considering station reports of precipitation, sea-level pressure (SLP)
   anomalies and two North Atlantic oscillation (NAO) indices. It is found
   that these relations have undergone consistent and simultaneous changes
   in the 20th century. Three characteristic periods can be identified.
   During 1900-25 and 1962-87, positive NINO3 index values are associated
   with enhanced precipitation over central Europe and reduced rainfall in
   southern Europe and northern Africa. The ENSO influence on precipitation
   over Scotland and Norway is small. The rainfall anomalies can be
   explained from the advective and dynamical implications of a north-south
   dipole in SLP correlations (warm ENSO events followed by low pressure in
   northern Europe and high pressure over the Mediterranean Sea-North
   Africa). This dipole hardly projects on the commonly used NAO centres
   (Iceland and Azores/Gibraltar) and thus ENSO-NAO correlations are
   insignificant. During 1931 -56 the NINO3 index reveals little influence
   on precipitation over the Iberian Peninsula and Morocco, but there are
   large negative correlations with precipitation over Scotland and Norway.
   This is related to an alteration of the NINO3-SLP correlation pattern,
   which implies high pressure over northern Europe and low pressure over
   central Europe after warm events, and thus a virtually inverted dipole
   with respect to the other two periods. The large westward extension of
   the dipole leads to a significant NAO-NINO3 correlation of r = -0.5.
   These alterations were accompanied by substantial large-scale
   circulation changes during the period 1931 -56, as revealed by
   anomalously high pressure and dry conditions over central-western
   Europe, a change in precipitation-producing SLP patterns for Morocco and
   an anomalously low number of positive NAO and NINO3 index values. It is
   left for discussion as to whether the decadal variations described are
   due to a change in the physics of the teleconnection or to stochastic
   fluctuations. Copyright (C) 2003 Royal Meteorological Society.}},
Publisher = {{WILEY}},
Address = {{111 RIVER ST, HOBOKEN 07030-5774, NJ USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Knippertz, P (Corresponding Author), Univ Wisconsin, Dept Atmospher \& Ocean Sci, 1225 W Dayton St, Madison, WI 53706 USA.
   Univ Cologne, Inst Geophys \& Meteorol, D-50923 Cologne, Germany.
   Univ Evora, Ctr Geofis Evora, P-7002554 Evora, Portugal.}},
DOI = {{10.1002/joc.944}},
ISSN = {{0899-8418}},
EISSN = {{1097-0088}},
Keywords = {{El Nino; NAO; Europe-North Africa; precipitation; sea-level pressure
   anomalies; decadal variability; running correlations; circulation
   changes}},
Keywords-Plus = {{SOUTHERN-OSCILLATION; ATMOSPHERIC CIRCULATION; SURFACE-TEMPERATURE;
   TROPICAL ATLANTIC; PRECIPITATION; VARIABILITY; ENSO; PRESSURE; PATTERNS;
   ANOMALIES}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{pknipp@meteor.wisc.edu}},
ResearcherID-Numbers = {{Ulbrich, Uwe/A-1070-2014
   Knippertz, Peter/D-5861-2016
   }},
ORCID-Numbers = {{Ulbrich, Uwe/0000-0001-7558-6622
   Knippertz, Peter/0000-0001-9856-619X
   Corte-Real, Joao Alexandre Medina/0000-0001-9624-4920}},
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Number-of-Cited-References = {{51}},
Times-Cited = {{73}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{13}},
Journal-ISO = {{Int. J. Climatol.}},
Doc-Delivery-Number = {{722DR}},
Unique-ID = {{ISI:000185360600002}},
DA = {{2020-08-06}},
}

@article{ ISI:000184879200001,
Author = {Galanti, E and Tziperman, E},
Title = {{A Midlatitude-ENSO teleconnection mechanism via baroclinically unstable
   long Rossby waves}},
Journal = {{JOURNAL OF PHYSICAL OCEANOGRAPHY}},
Year = {{2003}},
Volume = {{33}},
Number = {{9}},
Pages = {{1877-1888}},
Month = {{SEP}},
Abstract = {{The possibility of generating decadal ENSO variability via an ocean
   teleconnection to the midlatitude Pacific is studied. This is done by
   analyzing the sensitivity of the equatorial stratification to
   midlatitude processes using an ocean general circulation model, the
   adjoint method, and a quasigeostrophic normal-mode stability analysis.
   It is found that, on timescales of 2-15 yr, the equatorial Pacific is
   most sensitive to midlatitude planetary Rossby waves traveling from the
   midlatitudes toward the western boundary and then to the equator. Those
   waves that propagate through baroclinically unstable parts of the
   subtropical gyre are amplified by the baroclinic instability and
   therefore dominate the midlatitude signal arriving at the equator. This
   result implies that decadal variability in the midlatitude Pacific would
   be efficiently transmitted to the equatorial Pacific from specific areas
   of the midlatitude Pacific that are baroclinically unstable, such as the
   near-equatorial edges of the subtropical gyres (15degreesN and
   12degreesS). The Rossby waves that propagate via the baroclinically
   unstable areas are of the advective mode type, which follow the gyre
   circulation to some degree and arrive from as far as 25degreesN and
   30degreesS in the east Pacific. It is shown that the baroclinic
   instability amplifying these waves involves critical layers due to the
   vertical shear of the subtropical gyre circulation, at depths of 150-200
   m.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Galanti, E (Corresponding Author), Columbia Univ, Lamont Doherty Earth Observ, Int Res Inst Climate Predict, Earth Inst, Rm 202,Monell Bldg,61 Route 9W, Palisades, NY 10964 USA.
   Weizmann Inst Sci, IL-76100 Rehovot, Israel.}},
DOI = {{10.1175/1520-0485(2003)033<1877:AMTMVB>2.0.CO;2}},
ISSN = {{0022-3670}},
Keywords-Plus = {{NORTH PACIFIC; CLIMATE VARIABILITY; TROPICAL PACIFIC; OCEAN;
   THERMOCLINE; SENSITIVITY; MODEL; CONSTRUCTION; CIRCULATION; FREQUENCY}},
Research-Areas = {{Oceanography}},
Web-of-Science-Categories  = {{Oceanography}},
ORCID-Numbers = {{Galanti, Eli/0000-0002-5440-8779}},
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Number-of-Cited-References = {{36}},
Times-Cited = {{39}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{7}},
Journal-ISO = {{J. Phys. Oceanogr.}},
Doc-Delivery-Number = {{713VT}},
Unique-ID = {{ISI:000184879200001}},
DA = {{2020-08-06}},
}

@article{ ISI:000185037300008,
Author = {Adegbie, AT and Schneider, RR and Rohl, U and Wefer, G},
Title = {{Glacial millennial-scale fluctuations in central African precipitation
   recorded in terrigenous sediment supply and freshwater signals offshore
   Cameroon}},
Journal = {{PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY}},
Year = {{2003}},
Volume = {{197}},
Number = {{3-4}},
Pages = {{323-333}},
Month = {{SEP 1}},
Abstract = {{Evidence of rapid climatic oscillations like those observed in the
   Greenland ice cores and sediments from high latitudes of the northern
   Atlantic have been recognized in the pulses of terrigenous material to
   continental margin sediments off Cameroon. Fe/Ca ratios used as a
   parameter to quantify the relative proportions of terrigenous fluxes
   versus marine carbonate monitor the variability of the west African
   monsoon. They reveal the history of abrupt changes in precipitation over
   western and central Africa during the past 52 kyr. These rapid changes
   are particularly pronounced during the last glacial period and occur at
   timescales of a few thousand years. Stable oxygen isotope (delta(18)O)
   records of Globigerinoides ruber (pink) show high negative values
   reflecting periods of high monsoon precipitation. The Fe/Ca pattern is
   very similar to the Dansgaard-Oeschger cycles from the Greenland ice
   cores. The good correspondence between the warm interstadials of the
   Dansgaard-Oeschger cycles from the GISP2 ice core records and the high
   pulses of Fe/Ca sedimentation in our core suggest a strong
   teleconnection between the low-latitude African climate and the
   high-latitude northern hemisphere climate oscillations during the last
   glacial. This climatic link is probably vested in the west African
   monsoonal fluctuation that alters tropical sea surface temperatures,
   thermolialine circulations and in turn net export of heat from the south
   to the north Atlantic, coupled with the variability of the low-latitude
   southeast trade winds. (C) 2003 Elsevier B.V. All rights reserved.}},
Publisher = {{ELSEVIER SCIENCE BV}},
Address = {{PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Adegbie, AT (Corresponding Author), NIOMR, PMB 80108, Lagos, Nigeria.
   NIOMR, Lagos, Nigeria.
   Univ Bremen, Fachbereich Geowissensch, D-28359 Bremen, Germany.}},
DOI = {{10.1016/S0031-0182(03)00474-7}},
ISSN = {{0031-0182}},
Keywords = {{climate oscillation; Fe/Ca; last glacial period; stable oxygen isotopes;
   monsoon precipitation; Dansgaard-Oeschger cycles}},
Keywords-Plus = {{MILANKOVITCH CLIMATE VARIABILITY; SEA-SURFACE TEMPERATURES; EAST
   EQUATORIAL ATLANTIC; NORTH-ATLANTIC; PLANKTONIC-FORAMINIFERA;
   SOUTH-ATLANTIC; GREENLAND ICE; ICEBERG DISCHARGES; HEINRICH EVENTS;
   OCEAN}},
Research-Areas = {{Physical Geography; Geology; Paleontology}},
Web-of-Science-Categories  = {{Geography, Physical; Geosciences, Multidisciplinary; Paleontology}},
ResearcherID-Numbers = {{Gerold, Wefer/S-2291-2016
   Rohl, Ursula/G-5986-2011
   }},
ORCID-Numbers = {{Gerold, Wefer/0000-0002-6803-2020
   Rohl, Ursula/0000-0001-9469-7053
   Schneider, Ralph/0000-0003-1453-9181}},
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Number-of-Cited-References = {{77}},
Times-Cited = {{53}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{11}},
Journal-ISO = {{Paleogeogr. Paleoclimatol. Paleoecol.}},
Doc-Delivery-Number = {{716PJ}},
Unique-ID = {{ISI:000185037300008}},
DA = {{2020-08-06}},
}

@article{ ISI:000184929200014,
Author = {Ma, HM and Venkatesh, S and Jantunen, LM},
Title = {{Evidence of the impact of ENSO events on temporal trends of
   hexachlorobenzene air concentrations over the Great Lakes}},
Journal = {{SCIENCE OF THE TOTAL ENVIRONMENT}},
Year = {{2003}},
Volume = {{313}},
Number = {{1-3}},
Pages = {{177-184}},
Month = {{SEP 1}},
Abstract = {{This study presents an evidence for association of the air
   concentrations of HCB measured in the Great Lakes region with the El
   Nino-Southern Oscillation (ENSO) during the 1990s. The measured HCB
   concentrations in the atmosphere collected by the Integrated Atmospheric
   Deposition Network (IADN) program in the Great Lakes during the 1990s
   show strong correlations with the Multivariate ENSO index (MEI) during
   winter (December-February) and spring (March-May) seasons. These
   correlations are stronger in the western upper Great Lakes than in the
   eastern portion of the Great Lakes ecosystem (lake Ontario), and
   correspond well to the spatial variability of the surface air
   temperature in North America during El Nino years. Departures of HCB air
   concentrations for each winter during 1992-1999 from that averaged over
   all winters of 1992-1999, i.e. the anomaly, also show the same temporal
   trend as that of the MEI during the same period. In the same time
   period, it has been reported that direct HCB emissions from application
   of HCB in agriculture, from industrial sources in North America and in
   the rest of the world have decreased substantially compared to those in
   the 1970s and could not by themselves account for observed HCB air
   concentrations around the Great Lakes since the 1990s. Interannual
   fluctuations of HCB concentrations are caused most likely by reemission
   due to volatilization of HCB from the soil contaminated from past use,
   followed by long-range transport associated with ENSO events. In
   addition to the high correlation (R-2=0.61) between winter HCB air
   concentrations averaged over the Great Lakes region and the MEI the
   atmospheric circulation patterns associated with ENSO events are
   conducive to the long-range transport of HCB into the Great Lakes
   region. (C) 2003 Elsevier Science B.V. All rights reserved.}},
Publisher = {{ELSEVIER SCIENCE BV}},
Address = {{PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Ma, HM (Corresponding Author), Meteorol Serv Canada, Air Qual Res Branch, 4905 Dufferin St, Downsview, ON M3H 5T4, Canada.
   Meteorol Serv Canada, Air Qual Res Branch, Downsview, ON M3H 5T4, Canada.}},
DOI = {{10.1016/S0048-9697(03)00267-5}},
ISSN = {{0048-9697}},
Keywords = {{hexachlorobenzene (HCB); El Nino-Southern Oscillation (ENSO); great
   lakes; atmospheric teleconnection; Pacific/North American pattern (PNA);
   temporal trend}},
Keywords-Plus = {{SOUTHERN OSCILLATION; GEOPOTENTIAL

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