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Number-of-Cited-References = {{68}},
Times-Cited = {{32}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{18}},
Journal-ISO = {{Clim. Res.}},
Doc-Delivery-Number = {{741FQ}},
Unique-ID = {{ISI:000186448400004}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000183272300017,
Author = {Evans, ME and Rutter, NW and Catto, N and Chlachula, J and Nyvlt, D},
Title = {{Magnetoclimatology: Teleconnection between the Siberian loess record and
   North Atlantic Heinrich events}},
Journal = {{GEOLOGY}},
Year = {{2003}},
Volume = {{31}},
Number = {{6}},
Pages = {{537-540}},
Month = {{JUN}},
Abstract = {{New environmental magnetic data from loess and paleosol successions in
   outcrops in the upper reaches of the Ob River drainage, southern
   Siberia, track the major climatic variations over the last
   glacial-interglacial cycle. Profiles of magnetic susceptibility and
   alternating deposition of loess and soil-formation events correspond to
   oxygen isotope stages 1-5. The magnetic-susceptibility data, in
   association with the stratigraphic succession, confirm that the
   wind-vigor magnetoclimatological model is a viable alternative to the
   classic pedogenic model. Interpretation of magnetic-susceptibility data
   from loess-paleosol successions must therefore consider eolian dynamics,
   available source materials, and transport directions, in addition to
   pedogenic processes. Rapid magnetic fluctuations are also observed.
   These are identified-for the first time in Siberian records-as the
   signature of the abrupt cold pulses responsible for the. Heinrich layers
   in North Atlantic marine sediments. The data thus form a component of
   climatic teleconnections across the Northern Hemisphere, allowing
   correlations to be made among (1) Siberian magnetic susceptibility
   stratigraphy, (2) data recorded from other loess-paleosol successions in
   China, European Russia, Europe, and North America, (3) North Atlantic
   ice-rafted detritus, and (4) sea-surface temperatures derived from
   molecular stratigraphy of marine sediments off the northwest coast of
   Africa.}},
Publisher = {{GEOLOGICAL SOC AMER, INC}},
Address = {{PO BOX 9140, BOULDER, CO 80301-9140 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Evans, ME (Corresponding Author), Univ Alberta, Inst Geophys Res, Edmonton, AB T6G 2G1, Canada.
   Univ Alberta, Inst Geophys Res, Edmonton, AB T6G 2G1, Canada.
   Univ Alberta, Dept Earth \& Atmospher Sci, Edmonton, AB T6G 2E3, Canada.
   Mem Univ Newfoundland, Dept Geog, St John, NF A1B 3X9, Canada.
   Tech Univ Brno, Lab Palaeoecol, Zlin 76272, Czech Republic.
   Czech Geol Survey, Dept Quaternary Geol, Prague 11821 1, Czech Republic.}},
DOI = {{10.1130/0091-7613(2003)031<0537:MTBTSL>2.0.CO;2}},
ISSN = {{0016-8505}},
Keywords = {{loess; Siberia; paleoclimate; magnetic susceptibility; Heinrich events}},
Keywords-Plus = {{MAGNETIC-SUSCEPTIBILITY VARIATIONS; CHINESE LOESS; LATE QUATERNARY;
   PALEOCLIMATIC SIGNIFICANCE; PLEISTOCENE LOESS; HOLOCENE LOESS; ALASKAN
   LOESS; PALEOSOLS; PEDOGENESIS; DEPOSITION}},
Research-Areas = {{Geology}},
Web-of-Science-Categories  = {{Geology}},
Author-Email = {{evans@phys.ualberta.ca}},
ResearcherID-Numbers = {{Nyvlt, Daniel/J-6504-2019}},
ORCID-Numbers = {{Nyvlt, Daniel/0000-0002-6876-490X}},
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Number-of-Cited-References = {{39}},
Times-Cited = {{33}},
Usage-Count-Last-180-days = {{4}},
Usage-Count-Since-2013 = {{18}},
Journal-ISO = {{Geology}},
Doc-Delivery-Number = {{685PK}},
Unique-ID = {{ISI:000183272300017}},
DA = {{2020-08-06}},
}

@article{ ISI:000183298300008,
Author = {Spencer, H and Slingo, JM},
Title = {{The simulation of peak and delayed ENSO teleconnections}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2003}},
Volume = {{16}},
Number = {{11}},
Pages = {{1757-1774}},
Month = {{JUN}},
Abstract = {{There is much evidence that El Nino and La Nina lead to significant
   atmospheric seasonal predictability across much of the globe. However,
   despite successful predictions of tropical Pacific SSTs, atmospheric
   seasonal forecasts have had limited success. This study investigates
   model errors in the Hadley Centre Atmospheric Model version 3 (HadAM3)
   by analyzing composites of similar El Nino and La Nina events at their
   peak in December-January-February (DJF) and through their decay in
   March-April-May (MAM).
   The large-scale, tropical ENSO teleconnections are modeled accurately by
   HadAM3 during DJF but the strongest extratropical teleconnection, that
   in the North Pacific during winter, is modeled inaccurately. The
   Aleutian low is frequently observed to shift eastward during El Nino but
   the modeled response always consists of a deepening of the low without a
   shift. This is traced to small errors in the sensitivity of
   precipitation to SST in the tropical Pacific, which does not display
   enough variability so that the precipitation is always too high over the
   warmest SSTs. This error is reduced when vertical resolution is
   increased from 19 to 30 levels but enhanced horizontal resolution does
   not improve the simulation further.
   In MAM, following the peak of an El Nino or La Nina, atmospheric
   anomalies are observed to decay rapidly. The modeled ENSO response in
   DJF persists into MAM, making the extratropical anomalies in MAM too
   strong. This inaccuracy is again likely to be due to the high modeled
   sensitivity of tropical Pacific precipitation to SST, which is not
   significantly improved with enhanced vertical or horizontal resolution
   in MAM.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Spencer, H (Corresponding Author), Univ Reading, Dept Meteorol, Ctr Global Atmospher Modelling, Earley Gate,POB 243, Reading RG6 6BB, Berks, England.
   Univ Reading, Dept Meteorol, Ctr Global Atmospher Modelling, Reading RG6 6BB, Berks, England.}},
DOI = {{10.1175/1520-0442(2003)016<1757:TSOPAD>2.0.CO;2}},
ISSN = {{0894-8755}},
Keywords-Plus = {{SEA-SURFACE TEMPERATURE; MODEL INTERCOMPARISON PROJECT; TROPICAL
   CONVECTION; ATMOSPHERIC MODEL; EL-NINO; SEASONAL PREDICTABILITY; GCM
   SIMULATIONS; CLIMATE MODEL; VARIABILITY; ORGANIZATION}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
ResearcherID-Numbers = {{Weller, Hilary/A-1565-2011}},
ORCID-Numbers = {{Weller, Hilary/0000-0003-4553-7082}},
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Number-of-Cited-References = {{38}},
Times-Cited = {{43}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{2}},
Journal-ISO = {{J. Clim.}},
Doc-Delivery-Number = {{686AP}},
Unique-ID = {{ISI:000183298300008}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000183298300013,
Author = {Englehart, PJ and Douglas, AV},
Title = {{Assessing warm season drought episodes in the Central United States}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2003}},
Volume = {{16}},
Number = {{11}},
Pages = {{1831-1842}},
Month = {{JUN}},
Abstract = {{Recurrent drought episodes are a signature feature of the climate of the
   central United States. Using a particular set of definitions, this study
   examines some of the basic statistical features of previous drought
   episodes. It shows that there are distinct intraseasonal preferences for
   the onset of long periods of dry weather and that these preferences vary
   regionally in ways that are consistent with seasonal climate controls.
   Evaluation of past drought occurrences indicates that there is no simple
   or strong teleconnection between drought and the El Nino Southern
   Oscillation (ENSO) phenomenon. Individual drought episodes certainly
   evolve with unique character. However, based on analysis of large-scale
   variations in sea level pressure patterns, evidence is presented for
   systematic links between drought and the interdecadal climate mode often
   referred to as the Pacific decadal oscillation (PDO).}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Englehart, PJ (Corresponding Author), 3500 N 57th St, Kansas City, KS 66104 USA.
   Creighton Univ, Dept Atmospher \& Environm Sci, Omaha, NE 68178 USA.}},
DOI = {{10.1175/1520-0442(2003)016<1831:AWSDEI>2.0.CO;2}},
ISSN = {{0894-8755}},
EISSN = {{1520-0442}},
Keywords-Plus = {{SUMMER RAINFALL; SOIL-MOISTURE; GREAT-PLAINS; EL-NINO; PRECIPITATION;
   CLIMATE; OSCILLATION; TEMPERATURE; VARIABILITY; ENSO}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{pjenglehart@creighton.edu}},
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Number-of-Cited-References = {{55}},
Times-Cited = {{16}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{2}},
Journal-ISO = {{J. Clim.}},
Doc-Delivery-Number = {{686AP}},
Unique-ID = {{ISI:000183298300013}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000182607200005,
Author = {Fauchereau, N and Trzaska, S and Rouault, M and Richard, Y},
Title = {{Rainfall variability and changes in Southern Africa during the 20th
   century in the global warming context}},
Journal = {{NATURAL HAZARDS}},
Year = {{2003}},
Volume = {{29}},
Number = {{2}},
Pages = {{139-154}},
Month = {{JUN}},
Abstract = {{Rainfall variability and changes in Southern Africa over the 20th
   century are examined and their potential links to the global warming
   discussed. After a short review of the main conclusions of various
   experiments with Global Atmospheric Models (GCM) forced by increased
   concentrations of greenhouse gases for Southern Africa, a study of
   various datasets documents the observed changes in rainfall features at
   both daily and seasonal time steps through the last century.
   Investigations of daily rainfall parameters are so far limited to South
   Africa. They show that some regions have experienced a shift toward more
   extreme rainfall events in recent decades. Investigations of cumulative
   rainfall anomalies over the summer season do not show any trend to drier
   or moister conditions during the century. However, close examination
   reveals that rainfall variability in Southern Africa has experienced
   significant modifications, especially in the recent decades. Interannual
   variability has increased since the late 1960s. In particular, droughts
   became more intense and widespread. More significantly, teleconnection
   patterns associated with Southern African rainfall variability changed
   from regional before the 70s to near global after, and an increased
   statistical association to the El Nino-Southern Oscillation (ENSO)
   phenomenon is observed. Numerical experiments with a French GCM indicate
   that these changes in teleconnections could be related to long-term
   variations in the Sea-Surface-Temperature background, which are part of
   the observed global warming signal.}},
Publisher = {{SPRINGER}},
Address = {{ONE NEW YORK PLAZA, SUITE 4600, NEW YORK, NY, UNITED STATES}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Fauchereau, N (Corresponding Author), Univ Bourgogne, Ctr Rech Climatol, UMR CNRS 5080, Fac Sci Gabriel, 6 Bd Gabriel, F-21000 Dijon, France.
   Univ Bourgogne, Ctr Rech Climatol, UMR CNRS 5080, Fac Sci Gabriel, F-21000 Dijon, France.
   Univ Cape Town, Dept Oceanog, ZA-7700 Rondebosch, South Africa.}},
DOI = {{10.1023/A:1023630924100}},
ISSN = {{0921-030X}},
EISSN = {{1573-0840}},
Keywords = {{Southern Africa; rainfall variability; global warming; rainfall
   variability; teleconnections; ENSO; general circulation models}},
Keywords-Plus = {{RECENT CLIMATIC-CHANGE; EL-NINO; TEMPERATURE VARIABILITY;
   SURFACE-TEMPERATURE; EXTREME RAINFALL; ATMOSPHERE MODEL; SUMMER
   RAINFALL; PATTERNS; DROUGHTS; OSCILLATION}},
Research-Areas = {{Geology; Meteorology \& Atmospheric Sciences; Water Resources}},
Web-of-Science-Categories  = {{Geosciences, Multidisciplinary; Meteorology \& Atmospheric Sciences;
   Water Resources}},
Author-Email = {{nicolasf@u-bourgogne.fr}},
ResearcherID-Numbers = {{Rouault, Mathieu/A-5022-2008
   Richard, Yves/F-1874-2011}},
ORCID-Numbers = {{Rouault, Mathieu/0000-0002-3207-6777
   Richard, Yves/0000-0002-9203-0922}},
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Number-of-Cited-References = {{58}},
Times-Cited = {{150}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{29}},
Journal-ISO = {{Nat. Hazards}},
Doc-Delivery-Number = {{673XX}},
Unique-ID = {{ISI:000182607200005}},
DA = {{2020-08-06}},
}

@article{ ISI:000183177600008,
Author = {Rogers, JC and Coleman, JSM},
Title = {{Interactions between the Atlantic Multidecadal Oscillation, El Nino/La
   Nina, and the PNA in winter Mississippi valley stream flow}},
Journal = {{GEOPHYSICAL RESEARCH LETTERS}},
Year = {{2003}},
Volume = {{30}},
Number = {{10}},
Month = {{MAY 22}},
Abstract = {{{[}1] Winter streamgage data at 554 locations in the U. S. Geological
   Survey's Hydro-Climatic Data Network are used to evaluate interactions
   between the Atlantic multidecadal oscillation (AMO), the Pacific/North
   American (PNA) teleconnection pattern, and warm and cold equatorial
   Pacific Nino 3.4 events in producing Mississippi River basin discharge
   variations. The AMO is linked to statistically significant stream flow
   differences over the upper Mississippi Valley, as well as low (high)
   winter stream flow from 1930-1959 (1965-1994). Its influence in the
   lower Mississippi Valley is however not as apparent because of 4
   consecutive wet winters, 1949-1952, that disrupt the AMO warm/dry
   period. Persistent PNA zonal flow, and a La Nina event, occur during
   these winters and they are closely linked to high Tennessee and Ohio
   River valley stream levels. PNA-influenced stream flow on these rivers
   has a greater long-term winter impact on the lower Mississippi basin
   than does flow from the upper Mississippi.}},
Publisher = {{AMER GEOPHYSICAL UNION}},
Address = {{2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Rogers, JC (Corresponding Author), Ohio State Univ, Dept Geog, 1036 Derby Hall, Columbus, OH 43210 USA.
   Ohio State Univ, Dept Geog, Columbus, OH 43210 USA.}},
DOI = {{10.1029/2003GL017216}},
Article-Number = {{1518}},
ISSN = {{0094-8276}},
Keywords-Plus = {{SURFACE TEMPERATURE ANOMALIES; NORTH-AMERICAN PRECIPITATION;
   UNITED-STATES; RAINFALL; PACIFIC; TELECONNECTIONS}},
Research-Areas = {{Geology}},
Web-of-Science-Categories  = {{Geosciences, Multidisciplinary}},
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Number-of-Cited-References = {{13}},
Times-Cited = {{72}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{11}},
Journal-ISO = {{Geophys. Res. Lett.}},
Doc-Delivery-Number = {{683YA}},
Unique-ID = {{ISI:000183177600008}},
DA = {{2020-08-06}},
}

@article{ ISI:000183181200001,
Author = {Sankarasubramanian, A and Lall, U},
Title = {{Flood quantiles in a changing climate: Seasonal forecasts and causal
   relations}},
Journal = {{WATER RESOURCES RESEARCH}},
Year = {{2003}},
Volume = {{39}},
Number = {{5}},
Month = {{MAY 21}},
Abstract = {{{[}1] Recognizing that the frequency distribution of annual maximum
   floods at a given location may change over time in response to
   interannual and longer climate fluctuations, we compare two approaches
   for the estimation of flood quantiles conditional on selected ``climate
   indices'' that carry the signal of structured low-frequency climate
   variation, and influence the atmospheric mechanisms that modify local
   precipitation and flood potential. A parametric quantile regression
   approach and a semiparametric local likelihood approach are compared
   using synthetic data sets and for data from a streamflow gauging station
   in the western United States. Their relative utility in different
   settings for seasonal flood risk forecasting as well as for the
   assessment of long-term variation in flood potential is discussed.}},
Publisher = {{AMER GEOPHYSICAL UNION}},
Address = {{2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Sankarasubramanian, A (Corresponding Author), Columbia Univ, Lamont Doherty Earth Observ, Int Res Inst Climate Predict, Palisades, NY 10964 USA.
   Columbia Univ, Lamont Doherty Earth Observ, Int Res Inst Climate Predict, Palisades, NY 10964 USA.
   Columbia Univ, Dept Earth \& Environm Engn, New York, NY USA.}},
DOI = {{10.1029/2002WR001593}},
Article-Number = {{1134}},
ISSN = {{0043-1397}},
Keywords = {{teleconnection; seasonal flood forecasting; local likelihood; quantile
   regression}},
Keywords-Plus = {{NINO-SOUTHERN OSCILLATION; WESTERN UNITED-STATES; ENSO TELECONNECTIONS;
   REGRESSION QUANTILES; VARIABILITY; PRECIPITATION; DROUGHT; ASSOCIATIONS;
   MAGNITUDE; EXTREMES}},
Research-Areas = {{Environmental Sciences \& Ecology; Marine \& Freshwater Biology; Water
   Resources}},
Web-of-Science-Categories  = {{Environmental Sciences; Limnology; Water Resources}},
ResearcherID-Numbers = {{Lall, Upmanu/B-7992-2009}},
ORCID-Numbers = {{Lall, Upmanu/0000-0003-0529-8128}},
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Number-of-Cited-References = {{43}},
Times-Cited = {{73}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{18}},
Journal-ISO = {{Water Resour. Res.}},
Doc-Delivery-Number = {{683ZP}},
Unique-ID = {{ISI:000183181200001}},
DA = {{2020-08-06}},
}

@article{ ISI:000182635200060,
Author = {Nansai, K and Moriguchi, Y and Tohno, S},
Title = {{Compilation and application of Japanese inventories for energy
   consumption and air pollutant emissions using input-output tables}},
Journal = {{ENVIRONMENTAL SCIENCE \& TECHNOLOGY}},
Year = {{2003}},
Volume = {{37}},
Number = {{9}},
Pages = {{2005-2015}},
Month = {{MAY 1}},
Abstract = {{Preparing emission inventories is essential to the assessment and
   management of our environment. In this study, Japanese air pollutant
   emissions, energy consumption, and CO2 emissions categorized by
   approximately 400 sectors (as classified by Japanese input-output tables
   in 1995) were estimated, and the contributions of each sector to the
   total amounts were analyzed. The air pollutants examined were nitrogen
   oxides (NOX), sulfur oxides (SOX), and suspended particulate matter
   (SPM). Consumptions of about 20 fossil fuels and five other fuels were
   estimated according to sector. Air pollutant emission factors for
   stationary sources were calculated from the results of a survey on air
   pollution prevention in Japan. Pollutant emissions from mobile sources
   were estimated taking into consideration vehicle types, traveling
   speeds, and distances. This work also counted energy supply and
   emissions from seven nonfossil fuel sources, including nonthermal
   electric power, and CO2 emissions from limestone (for example, during
   cement production). The total energy consumption in 1995 was concluded
   to be 18.3 EJ, and the annual total emissions of CO2, NOX, SOX, and SPM
   were, respectively, 343 Mt-C, 3.51 Mt, 1.87 Mt, and 0.32 Mt. An
   input-output analysis of the emission inventories was used to calculate
   the amounts of energy consumption and emissions induced in each sector
   by the economic final demand.}},
Publisher = {{AMER CHEMICAL SOC}},
Address = {{1155 16TH ST, NW, WASHINGTON, DC 20036 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Nansai, K (Corresponding Author), Natl Inst Environm Studies, Endocrine Disruptors \& Dioxin Res Project, 16-2 Onogawa, Tsukuba, Ibaraki 3058506, Japan.
   Natl Inst Environm Studies, Endocrine Disruptors \& Dioxin Res Project, Tsukuba, Ibaraki 3058506, Japan.
   Natl Inst Environm Studies, Social \& Environm Syst Div, Tsukuba, Ibaraki 3058506, Japan.
   Kyoto Univ, Grad Sch Energy Sci, Kyoto 6110011, Japan.}},
DOI = {{10.1021/es0257669}},
ISSN = {{0013-936X}},
Keywords-Plus = {{SERVICES; GOODS}},
Research-Areas = {{Engineering; Environmental Sciences \& Ecology}},
Web-of-Science-Categories  = {{Engineering, Environmental; Environmental Sciences}},
ResearcherID-Numbers = {{Nansai, Keisuke/C-2516-2008
   }},
ORCID-Numbers = {{Tohno, Susumu/0000-0002-3936-5600}},
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Number-of-Cited-References = {{41}},
Times-Cited = {{46}},
Usage-Count-Last-180-days = {{2}},
Usage-Count-Since-2013 = {{32}},
Journal-ISO = {{Environ. Sci. Technol.}},
Doc-Delivery-Number = {{674KD}},
Unique-ID = {{ISI:000182635200060}},
DA = {{2020-08-06}},
}

@article{ ISI:000182538900011,
Author = {Rimbu, N and Lohmann, G and Felis, T and Patzold, J},
Title = {{Shift in ENSO teleconnections recorded by a northern Red Sea coral}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2003}},
Volume = {{16}},
Number = {{9}},
Pages = {{1414-1422}},
Month = {{MAY}},
Abstract = {{El Nino-Southern Oscillation (ENSO) teleconnections over Europe and the
   Middle East are evaluated using an oxygen isotope coral time series from
   the northern Red Sea and various instrumental datasets. A shift in the
   correlation between the Nino-3 index and the Red Sea coral record in the
   1970s is detected, and it is shown that this shift can be attributed to
   nonstationary circulation regimes and related ENSO teleconnections. It
   is found that positive anomalies of oxygen isotope in the Red Sea coral
   record from the middle 1930s to the late 1960s are associated with a
   strong Pacific-North Atlantic teleconnection accompanied by a weak
   Aleutian low, a more zonal flow at midlatitudes, and La Nina conditions
   in tropical Pacific. In contrast, positive anomalies of oxygen isotopes
   in the Red Sea coral after the 1970s are related to El Nino conditions
   and weaker Pan-Pacific Atlantic circulation regimes. Using the window
   correlation of the northern Red Sea coral record with two coral records
   from the tropical and subtropical Pacific, nonstationary relationships
   between the tropical Pacific and the European-Middle Eastern climate
   during the preinstrumental period are found. The results imply that the
   modulation of teleconnections at interdecadal timescales provides a
   limitation in the prediction and reconstruction of remote climate
   phenomena such as the ENSO impact over Europe.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Lohmann, G (Corresponding Author), Univ Bremen, Dept Geosci, PO 330 440, D-28334 Bremen, Germany.
   Univ Bremen, Dept Geosci, D-28334 Bremen, Germany.}},
DOI = {{10.1175/1520-0442-16.9.1414}},
ISSN = {{0894-8755}},
Keywords-Plus = {{NINO SOUTHERN OSCILLATION; EL-NINO; ATLANTIC OSCILLATION; CLIMATE
   VARIABILITY; GEOPOTENTIAL HEIGHT; PACIFIC; TEMPERATURE; WINTER; IMPACT;
   EUROPE}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
ResearcherID-Numbers = {{Felis, Thomas/N-2590-2019
   Felis, Thomas/G-6670-2011
   Lohmann, Gerrit/M-7453-2016
   Rimbu, Norel/C-4799-2011
   Patzold, Jurgen/D-5111-2017}},
ORCID-Numbers = {{Felis, Thomas/0000-0003-1417-9657
   Felis, Thomas/0000-0003-1417-9657
   Lohmann, Gerrit/0000-0003-2089-733X
   Rimbu, Norel/0000-0003-2832-9396
   Patzold, Jurgen/0000-0001-8074-4103}},
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Number-of-Cited-References = {{40}},
Times-Cited = {{33}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{7}},
Journal-ISO = {{J. Clim.}},
Doc-Delivery-Number = {{672TN}},
Unique-ID = {{ISI:000182538900011}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000183905100002,
Author = {Fernandez, J and Saenz, J and Zorita, E},
Title = {{Analysis of wintertime atmospheric moisture transport and its
   variability over southern Europe in the NCEP reanalyses}},
Journal = {{CLIMATE RESEARCH}},
Year = {{2003}},
Volume = {{23}},
Number = {{3}},
Pages = {{195-215}},
Month = {{APR 10}},
Abstract = {{A common analysis of instrumental monthly precipitation records and 6 h
   meteorological Reanalysis from the National Centers for Environmental
   Prediction (NCEP) was performed to diagnose the main modes of
   tropospheric, vertically integrated moisture transport over the
   Mediterranean basin and southern Europe. The moisture transport and its
   variability at each grid point and at the boundaries of the domain were
   quantified. Quantities such as the standard deviation of filtered
   geopotential height, one-point correlation maps and Z(300)-Z(500) and
   Z(500)-Z(700) thicknesses, related to the intensity and typical paths of
   baroclinic disturbances, were also computed to help in the
   interpretation of the results. It is clear that the leading mode of
   Mediterranean precipitation has its roots in the dynamics of the
   Atlantic storm track and the associated moisture transports. The second
   mode represents the internal redistribution of moisture inside the
   Mediterranean basin. Moisture is supplied to the atmosphere in the
   western Mediterranean, and this moisture is transported and precipitates
   over the eastern Mediterranean (mainly Turkey and Greece). Finally, the
   third mode depends on the role of European topography as a blocking
   factor for westerly moisture transport advected from the North Atlantic
   region.}},
Publisher = {{INTER-RESEARCH}},
Address = {{NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Fernandez, J (Corresponding Author), Univ Basque Country, Depto Fis Aplicada 2, Apdo 644, E-48080 Bilbao, Spain.
   Univ Basque Country, Depto Fis Aplicada 2, E-48080 Bilbao, Spain.
   GKSS Forschungszentrum Geesthacht GmbH, Inst Hydrophys, D-21502 Geesthacht, Germany.}},
DOI = {{10.3354/cr023195}},
ISSN = {{0936-577X}},
EISSN = {{1616-1572}},
Keywords = {{Mediterranean; southern Europe; precipitation; variability; winter;
   moisture}},
Keywords-Plus = {{NORTH-ATLANTIC OSCILLATION; CENTRAL UNITED-STATES; CLIMATE-CHANGE;
   TELECONNECTION PATTERNS; MEDITERRANEAN REGION; NASA/DAO REANALYSES;
   HYDROLOGICAL CYCLE; PRECIPITATION; RAINFALL; CIRCULATION}},
Research-Areas = {{Environmental Sciences \& Ecology; Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Environmental Sciences; Meteorology \& Atmospheric Sciences}},
Author-Email = {{chus@wm.lc.ehu.es}},
ResearcherID-Numbers = {{Saenz, Jon/A-7500-2011
   Fernandez, Jesus/F-5189-2011}},
ORCID-Numbers = {{Saenz, Jon/0000-0002-5920-7570
   Fernandez, Jesus/0000-0002-3483-0008}},
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Number-of-Cited-References = {{48}},
Times-Cited = {{52}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{8}},
Journal-ISO = {{Clim. Res.}},
Doc-Delivery-Number = {{696UC}},
Unique-ID = {{ISI:000183905100002}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000181578000003,
Author = {McEwan, PJ},
Title = {{Peer effects on student achievement: evidence from Chile}},
Journal = {{ECONOMICS OF EDUCATION REVIEW}},
Year = {{2003}},
Volume = {{22}},
Number = {{2}},
Pages = {{131-141}},
Month = {{APR}},
Abstract = {{This paper reports estimates of peer effects on student achievement,
   using a 1997 census of eighth-grade achievement in Chile. The-data allow
   detailed measures of peer characteristics to be constructed for each
   classroom within a school. The paper addresses the endogeneity of peer
   variables by including school fixed effects that control for unobserved
   family and student characteristics. The estimates suggest that the
   classroom mean of mothers' education is an important determinant of
   individual achievement, though subject to diminishing marginal returns.
   Additional specifications using family fixed effects are not suggestive
   that estimates are biased by within-school sorting. (C) 2002 Elsevier
   Science Ltd. All rights reserved.}},
Publisher = {{PERGAMON-ELSEVIER SCIENCE LTD}},
Address = {{THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{McEwan, PJ (Corresponding Author), Wellesley Coll, Dept Econ, 106 Cent St, Wellesley, MA 02481 USA.
   Wellesley Coll, Dept Econ, Wellesley, MA 02481 USA.}},
DOI = {{10.1016/S0272-7757(02)00005-5}},
ISSN = {{0272-7757}},
Keywords = {{input output analysis; peer effects; Chile; achievement}},
Keywords-Plus = {{MOBILITY EXPERIMENT; PUBLIC-SCHOOLS; PRIVATE; IMPACT; DIFFERENCE;
   OUTCOMES}},
Research-Areas = {{Business \& Economics; Education \& Educational Research}},
Web-of-Science-Categories  = {{Economics; Education \& Educational Research}},
ResearcherID-Numbers = {{McEwan, Patrick J./G-4547-2012
   }},
ORCID-Numbers = {{McEwan, Patrick/0000-0002-3095-2948}},
Cited-References = {{Aaronson D, 1998, J HUM RESOUR, V33, P915, DOI 10.2307/146403.
   ASHENFELTER O, 1994, AM ECON REV, V84, P1157.
   BRYK A, 1988, UNPUB HIGH SCH COMMU.
   Caldas SJ, 1997, J EDUC RES, V90, P269, DOI 10.1080/00220671.1997.10544583.
   Coleman J.S., 1966, EQUALITY ED OPPORTUN.
   CURRIE J, 1995, AM ECON REV, V85, P341.
   DUNCAN GJ, 1997, NEIGHBORHOOD POVERTY, V1, P219.
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   EVANS WN, 1992, J POLIT ECON, V100, P966, DOI 10.1086/261848.
   GAVIRIA A, 1997, UNPUB SCH BASED PEER.
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   HANUSHEK EA, 1998, 6691 NAT BUR EC RES.
   HENDERSON V, 1978, J PUBLIC ECON, V10, P97, DOI 10.1016/0047-2727(78)90007-5.
   HOXBY CM, 2000, 7867 NAT BUR EC RES.
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   Katz LF, 2001, Q J ECON, V116, P607, DOI 10.1162/00335530151144113.
   Link C. R., 1991, ECON EDUC REV, V10, P297, DOI DOI 10.1016/0272-7757(91)90020-P.
   Ludwig J, 2001, Q J ECON, V116, P655, DOI 10.1162/00335530151144122.
   Manski C. F., 1992, ECON EDUC REV, V11, P351.
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   MAYER SE, 1991, URBAN UNDERCLASS, P321.
   McEwan P., 2001, ED EC, V9, P103, DOI DOI 10.1080/09645290110056958.
   McEwan PJ, 2000, EDUC EVAL POLICY AN, V22, P213, DOI 10.3102/01623737022003213.
   McEwan PJ, 2000, REV EDUC RES, V70, P103, DOI 10.2307/1170659.
   Moffitt R., 2001, SOCIAL DYNAMICS.
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   Nechyba T., 1999, IMPACT FAMILY COMMUN.
   ROBERTSON D, 1996, 311 CTR EC PERF LOND.
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   SUMMERS AA, 1977, AM ECON REV, V67, P639.
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   WILLMS JD, 1986, AM SOCIOL REV, V51, P224, DOI 10.2307/2095518.
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   Zimmer RW, 2000, J POLICY ANAL MANAG, V19, P75, DOI 10.1002/(SICI)1520-6688(200024)19:1<75::AID-PAM5>3.0.CO;2-W.
   ZIMMERMAN D, 1999, UNPUB PEER EFFECTS A.}},
Number-of-Cited-References = {{36}},
Times-Cited = {{111}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{19}},
Journal-ISO = {{Econ. Educ. Rev.}},
Doc-Delivery-Number = {{655XM}},
Unique-ID = {{ISI:000181578000003}},
DA = {{2020-08-06}},
}

@article{ ISI:000183140200005,
Author = {Dieter, M and Thoroe, C},
Title = {{Forestry and forest industry sector in the Federal Republic of Germany
   according to the new European-Wide sector definition}},
Journal = {{FORSTWISSENSCHAFTLICHES CENTRALBLATT}},
Year = {{2003}},
Volume = {{122}},
Number = {{2}},
Pages = {{138-151}},
Month = {{APR}},
Abstract = {{The European Parliament has extended its forest industry sector
   definition to be applied for official reporting. According to this
   definition, the forest industry encompasses wood processing industries,
   pulp, paper and paperboard industries and newly, printing and publishing
   industries as well. Statistically, the forestry and forest industry
   sector becomes much more important with it. In the year 1997, nearly one
   million people have worked in about 90,000 companies in the forestry and
   forest industry sector in the Federal Republic of Germany. They have
   gained a production value of about 100 milliard EUR. Nevertheless the
   forestry and forest industry sector still shares only 3\% in the entire
   national economy, respective of if the number of working people or the
   production value is used as criterions. A comparative analysis shows
   that the use of the relatively rough systematic of the National
   Accounting leads to a very similar result as compared to the use of more
   detailed sector specific statistics.
   On the basis of the Input-Output-Tables - the most recent ones are
   available for the year 1997- the internal and external integration of
   the forestry and forest industry sector can be analysed. It can be shown
   that intermediate consumption is dominating, both at the input and at
   the output side. More than 60\% of the forestry and forest industry
   sector output is used as input in the domestic production process.
   Nonetheless the input is not of high importance for any other sector.
   Significant input-coefficients show the pulp and paper products for
   paper articles as well as the printing products for publishers'
   products. For the entire pulp and paper industry high import- as well as
   export-coefficients have been found. This points at a distinct
   international division of labour in this sector. The inverse
   coefficients are relatively low. Thus an overall increase in end use
   demand would lead only to a slight momentum for the forestry and forest
   industry sector.}},
Publisher = {{BLACKWELL VERLAG GMBH}},
Address = {{KURFURSTENDAMM 57, D-10707 BERLIN, GERMANY}},
Type = {{Article}},
Language = {{German}},
Affiliation = {{Thoroe, C (Corresponding Author), Bundesforsch Anstalt Forst \& Holzwirtschaft, Inst Okon, Leuschnerstr 91, D-21031 Hamburg, Germany.
   Bundesforsch Anstalt Forst \& Holzwirtschaft, Inst Okon, D-21031 Hamburg, Germany.}},
ISSN = {{0015-8003}},
Keywords = {{forestry and forest industry sector; sector definition; structure
   analysis; National Accounting; Input-Output-Analysis}},
Research-Areas = {{Forestry}},
Web-of-Science-Categories  = {{Forestry}},
Cited-References = {{BARTELHEIMER P, 1976, FORSTWISSENSCHAFTLIC, P79.
   MOOG M, 1987, EIGNUNG QUANTITATIVE, V29.
   {*}STBA, 1999, BETR ARB LAND FORSTW.
   {*}STBA, 2000, VOLKSW GES KONT STAN.
   {*}STBA, 1997, BESCH UMS EN UNT BET.
   {*}STBA, 1997, BETR BESCH UMS VER G.
   {*}STBA, 2000, WIRTSCH STAT, P377.
   {*}STBA, 1997, AUSS WAR LAND.
   {*}STBA, 1997, INP OUTP TAB 1997 BU.
   {*}STBA, 1995, ERGEB

license_type: permissive

branch_name: refs/heads/master

extension: bib