text:
NISSE UNTERNEHM.
   {*}STBA HAND GASTST, 1993, GROSS HAND.
   THOROE C, 1998, BEIYTRAGE FORSTOKONO, V31.}},
Number-of-Cited-References = {{12}},
Times-Cited = {{5}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{8}},
Journal-ISO = {{Forstwiss. Cent.bl.}},
Doc-Delivery-Number = {{683GN}},
Unique-ID = {{ISI:000183140200005}},
DA = {{2020-08-06}},
}

@article{ ISI:000182449500003,
Author = {Lau, KM and Zhou, JY},
Title = {{Anomalies of the South American summer monsoon associated with the
   1997-99 El Nino southern oscillation}},
Journal = {{INTERNATIONAL JOURNAL OF CLIMATOLOGY}},
Year = {{2003}},
Volume = {{23}},
Number = {{5}},
Pages = {{529-539}},
Month = {{APR}},
Abstract = {{We describe the rainfall and circulation anomalies of the South American
   summer monsoon (SASM) during December-January-February (DJF) of 1997-98
   (El Nino) and 1998-99 (La Nina). The most pronounced rainfall signals in
   DJF 1997-98 include (a) excessive rainfall over northern Peru and
   Ecuador, (b) deficient rainfall over northern and central Brazil, and
   (c) above-normal rainfall over southeastern subtropical South America.
   The rainfall anomalies in (a) and (b) are associated with the excitation
   of an anomalous east-west overturning cell with rising motion and
   low-level westerlies over the equatorial eastern Pacific, coupled to
   sinking motion and low-level easterlies over northern Brazil. The
   easterlies turn sharply southeastward on encountering the steep
   topography of the Andes, enhancing the summertime low-level jet (LLJ)
   along the eastern foothills of the Andes near 15-20degreesS, possibly
   contributing to the increased rainfall in (c).
   During DJF 1997-98, the sea-surface temperature-induced warming spreads
   and expands over the entire tropical troposphere. The eastward expansion
   of a warm upper tropospheric geopotential and temperature ridge from the
   Nino-3 region, across subtropical South America to the southeast
   Atlantic, enhances warming over the Altiplano Plateau, hydrostatically
   strengthening the Bolivia high. Similar to previous warming events, the
   South Pacific high is weakened, and the South Atlantic high is
   strengthened. During DJF 1998-99, as cold water develops over the
   equatorial central Pacific, the SASM anomalies in the tropics are weaker
   and less organized and appear to be in transition to the opposite phase
   to those found in DJF 97-98. In the subtropics, notable features include
   a weakening of the LLJ, a rainfall pattern associated with a poleward
   shift of the South Atlantic convergence zone, and development of the
   Pacific-South America teleconnection pattern. Published in 2003 by John
   Wiley Sons, Ltd.}},
Publisher = {{WILEY}},
Address = {{111 RIVER ST, HOBOKEN 07030-5774, NJ USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Lau, KM (Corresponding Author), NASA, Goddard Space Flight Ctr, Atmospheres Lab, Code 910, Greenbelt, MD 20771 USA.
   NASA, Goddard Space Flight Ctr, Atmospheres Lab, Greenbelt, MD 20771 USA.
   Univ Maryland, Goddard Earth Sci \& Technol Ctr, Baltimore, MD 21250 USA.}},
DOI = {{10.1002/joc.900}},
ISSN = {{0899-8418}},
EISSN = {{1097-0088}},
Keywords = {{ENSO; South American summer monsoon; interannual variability; low-level
   jets}},
Keywords-Plus = {{SEA-SURFACE TEMPERATURE; TROPICAL ATLANTIC; INTERANNUAL VARIABILITY;
   NORTHEAST BRAZIL; RAINFALL; PRECIPITATION; CIRCULATION; CLIMATE;
   DYNAMICS; MODES}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{lau@climate.gsfc.nasa.gov}},
ResearcherID-Numbers = {{Lau, William K/E-1510-2012}},
ORCID-Numbers = {{Lau, William K/0000-0002-3587-3691}},
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Number-of-Cited-References = {{32}},
Times-Cited = {{23}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{14}},
Journal-ISO = {{Int. J. Climatol.}},
Doc-Delivery-Number = {{671DF}},
Unique-ID = {{ISI:000182449500003}},
DA = {{2020-08-06}},
}

@article{ ISI:000182108000001,
Author = {Wu, L and Liu, Z and Gallimore, R and Jacob, R and Lee, D and Zhong, Y},
Title = {{Pacific decadal variability: The tropical Pacific mode and the North
   Pacific mode}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2003}},
Volume = {{16}},
Number = {{8}},
Pages = {{1101-1120}},
Month = {{APR}},
Abstract = {{Pacific decadal variability is studied in a series of coupled global
   ocean - atmosphere simulations aided by two ``modeling surgery''
   strategies: partial coupling ( PC) and partial blocking ( PB). The PC
   experiments retain full ocean - atmosphere coupling in selected regions,
   but constrain ocean - atmosphere coupling elsewhere by prescribing the
   model climatological SST to force the atmospheric component of the
   coupled system. In PB experiments, sponge walls are inserted into the
   ocean component of the coupled model at specified latitudinal bands to
   block the extratropical - tropical oceanic teleconnection.
   Both modeling and observational studies suggest that Pacific decadal
   variability is composed of two distinct modes: a decadal to bidecadal
   tropical Pacific mode ( TPM) and a multidecadal North Pacific mode (
   NPM). The PC and PB experiments showed that the tropical Pacific mode
   originates predominantly from local coupled ocean - atmosphere
   interaction within the tropical Pacific. Extratropical - tropical
   teleconnections, although not a necessary precondition for the genesis
   of the tropical decadal variability, can enhance SST variations in the
   Tropics. The decadal memory in the Tropics seems to be associated with
   tropical higher baroclinic modes. The North Pacific mode originates from
   local atmospheric stochastic processes and coupled ocean - atmosphere
   interaction. Atmospheric stochastic forcing can generate a weaker
   NPM-like pattern in both the atmosphere and ocean, but with no preferred
   timescales. In contrast, coupled ocean - atmosphere feedback can enhance
   the variability substantially and generate a basin-scale multidecadal
   mode in the North Pacific. The multidecadal memory in the midlatitudes
   seems to be associated with the delayed response of the
   subtropical/subpolar gyre to wind stress variation in the central North
   Pacific and the slow growing/decaying of SST anomalies that propagate
   eastward in the Kuroshio Extension region. Oceanic dynamics,
   particularly the advection of the mean temperature by anomalous
   meridional surface Ekman flow and western boundary currents, plays an
   important role in generating the North Pacific mode.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Wu, L (Corresponding Author), Univ Wisconsin, Ctr Climat Res, 1225 W Dayton St, Madison, WI 53706 USA.
   Univ Wisconsin, Ctr Climat Res, Madison, WI 53706 USA.
   Argonne Natl Lab, Argonne, IL 60439 USA.}},
DOI = {{10.1175/1520-0442(2003)16<1101:PDVTTP>2.0.CO;2}},
ISSN = {{0894-8755}},
EISSN = {{1520-0442}},
Keywords-Plus = {{OCEAN-ATMOSPHERE INTERACTION; SEA-SURFACE TEMPERATURES; CLIMATE
   VARIABILITY; SST ANOMALIES; ENSO; OSCILLATION; SYSTEM; MIDLATITUDES;
   DYNAMICS; ORIGINS}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{lxw@tuna.meteor.wisc.edu}},
ResearcherID-Numbers = {{Jacob, Robert/D-2580-2011
   }},
ORCID-Numbers = {{Jacob, Robert/0000-0002-9444-6593
   Lee, dong eun/0000-0001-8546-563X}},
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Number-of-Cited-References = {{61}},
Times-Cited = {{125}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{27}},
Journal-ISO = {{J. Clim.}},
Doc-Delivery-Number = {{665FB}},
Unique-ID = {{ISI:000182108000001}},
DA = {{2020-08-06}},
}

@article{ ISI:000182108000002,
Author = {Watanabe, M and Jin, FF},
Title = {{A moist linear baroclinic model: Coupled dynamical-convective response
   to El Nino}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2003}},
Volume = {{16}},
Number = {{8}},
Pages = {{1121-1139}},
Month = {{APR}},
Abstract = {{A newly developed, linear baroclinic model ( LBM) and its application to
   the tropical ENSO teleconnection is described. The model, based on
   primitive equations linearized about the observed, zonally varying basic
   state in northern winter, involves linear schemes for the cumulus
   convection, and surface sensible and latent heat fluxes, referred to as
   the moist LBM. This enables us to solve a steady-state response of the
   coupled dynamical convective system to a given SST anomaly, which is
   fairly different from the conventional dry LBM. Linear representation of
   the convection is acceptable for a realistic range of SST anomalies,
   reproducing well the Rossby wave train computed in the conventional LBM
   forced by a tropical heating.
   The moist LBM is used to examine the formation mechanisms of an
   anomalous low-level anticyclone near the Philippines that links El Nino
   with the Asian winter monsoon. Given that the conventional LBM simulates
   the Philippine Sea anticyclone as a Rossby response to the anomalous
   diabatic cooling associated with the weakened convection over the
   Maritime Continent, causes of the convective suppression are examined.
   Moist LBM experiments forced by observed El Nino SST anomalies indicate
   that a basinwide warming of the Indian Ocean, in addition to SST
   anomalies in the Pacific, has a considerable impact in weakening the
   convection over the Maritime Continent through a modulation of the
   Walker circulation. Observational analysis supports this idea and
   further suggests that the lagged Indian Ocean response to El Nino
   contributes to determining when the Philippine Sea anticyclone is
   developed. The moist LBM identified a positive wind-evaporation feedback
   at work between the Philippine anticyclone and the western Pacific SST
   anomaly, which might also contribute.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Watanabe, M (Corresponding Author), Hokkaido Univ, Div Ocean \& Atmospher Sci, Nishi 5,Kita 10, Sapporo, Hokkaido 0600810, Japan.
   Hokkaido Univ, Div Ocean \& Atmospher Sci, Sapporo, Hokkaido 0600810, Japan.
   Univ Hawaii Manoa, Sch Ocean \& Earth Sci \& Technol, Dept Meteorol, Honolulu, HI 96822 USA.}},
DOI = {{10.1175/1520-0442(2003)16<1121:AMLBMC>2.0.CO;2}},
ISSN = {{0894-8755}},
Keywords-Plus = {{SEA-SURFACE TEMPERATURE; FREQUENCY INTRASEASONAL OSCILLATIONS;
   MADDEN-JULIAN OSCILLATION; ASIAN SUMMER MONSOON; WAVE-CISK;
   SOUTHERN-OSCILLATION; INTERANNUAL VARIATIONS; TROPICAL VARIABILITY;
   AUSTRALIAN MONSOONS; ADJUSTMENT SCHEME}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
ResearcherID-Numbers = {{Watanabe, Masahiro/G-8228-2017}},
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Number-of-Cited-References = {{49}},
Times-Cited = {{78}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{29}},
Journal-ISO = {{J. Clim.}},
Doc-Delivery-Number = {{665FB}},
Unique-ID = {{ISI:000182108000002}},
DA = {{2020-08-06}},
}

@article{ ISI:000182108000004,
Author = {Cazes-Boezio, G and Robertson, AW and Mechoso, CR},
Title = {{Seasonal dependence of ENSO teleconnections over South America and
   relationships with precipitation in Uruguay}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2003}},
Volume = {{16}},
Number = {{8}},
Pages = {{1159-1176}},
Month = {{APR}},
Abstract = {{The El Nino-Southern Oscillation ( ENSO) has an established impact on
   precipitation in Uruguay during austral spring ( October-December). This
   impact is absent in peak summer ( January-February), and returns weakly
   in fall winter ( March-July). Interannual and intraseasonal variability
   of the atmospheric circulation over South America and the South Pacific
   is investigated using the NCEP-NCAR reanalysis data for these seasons.
   The leading empirical orthogonal function ( EOF) of seasonally averaged
   200-hPa winds over South America is found to be associated with ENSO
   through a pronounced Walker cell component in all seasons. However,
   during spring, this pattern acquires an extratropical teleconnection
   that links the circulation over southeastern South America ( SESA) with
   ENSO. This extratropical teleconnection disappears in summer, when the
   circulation over SESA is dominated by variability in the South Atlantic
   convergence zone. In fall, extratropical South America again becomes
   affected by a wavelike pattern that extends over the South Pacific, but
   it is uncorrelated with ENSO.
   On intraseasonal timescales, a cluster analysis of daily geopotential
   height fields over the South Pacific sector reveals three wave
   train-like circulation regimes with similar structures in all seasons.
   During the transition seasons ( but not summer), the frequencies of
   occurrence of two of these regimes are found to be significantly
   different from normal in years when the interannual wavelike EOFs are
   pronounced. Interannual anomaly patterns are constructed from the
   intraseasonal regimes according to these changes in their frequency of
   occurrence, and shown to resemble quite closely the interannual EOFs
   over the South Pacific sector. These results provide evidence that the
   interannual teleconnection patterns seen over the South Pacific in
   austral spring and fall-winter are due to changes in the frequency of
   occurrence and amplitude of intraseasonal circulation regimes. The
   Rossby wave source composited over ENSO years suggests that ENSO heating
   anomalies are able to trigger these changes in regime occurrence and
   amplitude during October-December through Rossby wave propagation,
   leading to the known ENSO teleconnection in austral spring. By contrast,
   the interannual teleconnection over the South Pacific during fall-winter
   appears to be due to essentially random changes in the frequency of
   occurrence of the intraseasonal circulation regimes, which are found to
   be much larger than during austral summer when no extratropical
   teleconnection pattern exists.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Cazes-Boezio, G (Corresponding Author), Univ Republica, Fac Ingn, Inst Mecan Fluidos \& Ingn Ambiental Prof Ing Osca, Julio Herrera \& Reissig 565, Montevideo 11300, Uruguay.
   Univ Republica, Fac Ingn, Inst Mecan Fluidos \& Ingn Ambiental Prof Ing Osca, Montevideo 11300, Uruguay.
   Univ Calif Los Angeles, Dept Atmospher Sci, Los Angeles, CA 90024 USA.}},
DOI = {{10.1175/1520-0442(2003)16<1159:SDOETO>2.0.CO;2}},
ISSN = {{0894-8755}},
Keywords-Plus = {{ATLANTIC CONVERGENCE ZONE; NORTHERN-HEMISPHERE WINTER; SEA-SURFACE
   TEMPERATURE; EL-NINO; PERSISTENT ANOMALIES; WEATHER REGIMES; HEIGHT
   FIELD; VARIABILITY; CIRCULATION; CLIMATE}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
ResearcherID-Numbers = {{Robertson, Andrew W/H-7138-2015}},
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Number-of-Cited-References = {{39}},
Times-Cited = {{77}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{4}},
Journal-ISO = {{J. Clim.}},
Doc-Delivery-Number = {{665FB}},
Unique-ID = {{ISI:000182108000004}},
DA = {{2020-08-06}},
}

@article{ ISI:000182108000010,
Author = {Hanley, DE and Bourassa, MA and O'Brien, JJ and Smith, SR and Spade, ER},
Title = {{A quantitative evaluation of ENSO indices}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2003}},
Volume = {{16}},
Number = {{8}},
Pages = {{1249-1258}},
Month = {{APR}},
Abstract = {{El Nino-Southern Oscillation ( ENSO) is a natural, coupled
   atmospheric-oceanic cycle that occurs in the tropical Pacific Ocean on
   an approximate timescale of 2-7 yr. ENSO events have been shown in
   previous studies to be related to regional extremes in weather ( e. g.,
   hurricane occurrences, frequency and severity of tornadoes, droughts,
   and floods). The teleconnection of ENSO events to extreme weather events
   means that the ability to classify an event as El Nino or La Nina is of
   interest in scientific and other applications.
   ENSO is most often classified using indices that indicate the warmth and
   coolness of equatorial tropical Pacific Ocean sea surface temperatures (
   SSTs). Another commonly used index is based on sea level pressure
   differences measured across the tropical Pacific Ocean. More recently,
   other indices have been proposed and have been shown to be effective in
   describing ENSO events. There is currently no consensus within the
   scientific community as to which of many indices best captures ENSO
   phases. The goal of this study is to compare several commonly used ENSO
   indices and to determine whether or not one index is superior in
   defining ENSO events; or alternatively, to determine which indices are
   best for various applications.
   The response and sensitivity of the SST-based indices and pressure-based
   indices are compared. The Nino-4 index has a relatively weak response to
   El Nino; the Nino-1+2 index has a relatively strong response to La Nina.
   Analysis of the sensitivity of the indices relative to one another
   suggests that the choice of index to use in ENSO studies is dependent
   upon the phase of ENSO that is to be studied. The Japan Meteorological
   Agency ( JMA) index is found to be more sensitive to La Nina events than
   all other indices. The Southern Oscillation, Nino-3.4, and Nino-4
   indices are almost equally sensitive to El Nino events and are more
   sensitive than the JMA, Nino-1+2, and Nino-3 indices.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Hanley, DE (Corresponding Author), Div Forestry, 3125 Conner Blvd, Tallahassee, FL 32399 USA.
   Florida State Univ, Ctr Ocean Atmospher Predict Studies, Tallahassee, FL 32306 USA.}},
DOI = {{10.1175/1520-0442(2003)16<1249:AQEOEI>2.0.CO;2}},
ISSN = {{0894-8755}},
Keywords-Plus = {{SOUTHERN OSCILLATION; EL-NINO; OCEAN; EVOLUTION; PRESSURE; PACIFIC;
   INDEXES; SST}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
ResearcherID-Numbers = {{Bourassa, Mark/Z-2428-2019}},
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Number-of-Cited-References = {{21}},
Times-Cited = {{124}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{30}},
Journal-ISO = {{J. Clim.}},
Doc-Delivery-Number = {{665FB}},
Unique-ID = {{ISI:000182108000010}},
DA = {{2020-08-06}},
}

@article{ ISI:000181647000004,
Author = {Pekarova, P and Miklanek, P and Pekar, J},
Title = {{Spatial and temporal runoff oscillation analysis of the main rivers of
   the world during the l9th-20th centuries}},
Journal = {{JOURNAL OF HYDROLOGY}},
Year = {{2003}},
Volume = {{274}},
Number = {{1-4}},
Pages = {{62-79}},
Month = {{APR 1}},
Abstract = {{The annual discharge time series of selected large rivers in the world
   were tested for wet and dry periods. The 28-29-years cycle, as well as
   20-22-years cycle of extremes occurrence were identified. From the trend
   analysis it follows that the hydrological characteristics of the rivers
   must be stated at least for one 28-year period. If we want to identify
   any trend uninfluenced by the 28-year periodicity of the discharge time
   series, we must determine the trend during a single or multiple curve
   cycle, starting and terminating by either minima (e.g. 1861-1946 in
   West/Central Europe) or maxima (e.g. 1847-1930 or 1931-1984 in
   West/Central Europe). Trends determined for other periods are influenced
   by the periodicity of the series and depend on the position of the
   starting point on the increasing or recession curve. Long-term trends
   during the period 1860-1990 have not been detected for the West/Central
   European runoff. Further, the temporal shift in the discharge extremes
   occurrence (both, maxima and minima) was shown to depend on the
   longitude and latitude. The time shift between Neva and Amur discharge
   time series is about four years, between Amur and St Lawrence is about
   16 years, and between St. Lawrence and Neva is about nine years. The
   time shift between Congo and Amazon is about seven years. (C) 2003
   Elsevier Science B.V. All rights reserved.}},
Publisher = {{ELSEVIER}},
Address = {{RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Pekarova, P (Corresponding Author), Slovak Acad Sci, Inst Hydrol, Racianska 75, Bratislava 83811, Slovakia.
   Slovak Acad Sci, Inst Hydrol, Bratislava 83811, Slovakia.
   Comenius Univ, Dept Econ \& Financial Models, Bratislava 84248, Slovakia.}},
DOI = {{10.1016/S0022-1694(02)00397-9}},
Article-Number = {{PII S0022-1694(02)00397-9}},
ISSN = {{0022-1694}},
EISSN = {{1879-2707}},
Keywords = {{long-term runoff fluctuation; discharge; time series analysis; spectral
   analysis; temporal pattern; teleconnection}},
Keywords-Plus = {{ENSO}},
Research-Areas = {{Engineering; Geology; Water Resources}},
Web-of-Science-Categories  = {{Engineering, Civil; Geosciences, Multidisciplinary; Water Resources}},
Author-Email = {{pekarova@uh.savba.sk
   miklanek@uh.savba.sk
   pekar@fmph.uniba.sk}},
ResearcherID-Numbers = {{Pekarova, Pavla/S-7400-2017}},
ORCID-Numbers = {{Pekarova, Pavla/0000-0002-1180-2215}},
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Number-of-Cited-References = {{24}},
Times-Cited = {{95}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{10}},
Journal-ISO = {{J. Hydrol.}},
Doc-Delivery-Number = {{657CC}},
Unique-ID = {{ISI:000181647000004}},
DA = {{2020-08-06}},
}

@article{ ISI:000181375800050,
Author = {Rybski, D and Havlin, S and Bunde, A},
Title = {{Phase synchronization in temperature and precipitation records}},
Journal = {{PHYSICA A-STATISTICAL MECHANICS AND ITS APPLICATIONS}},
Year = {{2003}},
Volume = {{320}},
Pages = {{601-610}},
Month = {{MAR 15}},
Abstract = {{We study phase synchronization between atmospheric variables such as
   daily mean temperature and daily precipitation records. We find
   significant phase synchronization between records of Oxford and Vienna
   as well as between the records of precipitation and temperature in each
   city. To find the time delay in the synchronization between the records
   we study the time lag phase synchronization when the records are shifted
   by a variable time interval of days. We also compare the results of the
   method with the classical cross-correlation method and find that in
   certain cases the phase synchronization yields more significant results.
   (C) 2002 Elsevier Science B.V. All rights reserved.}},
Publisher = {{ELSEVIER SCIENCE BV}},
Address = {{PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Rybski, D (Corresponding Author), Univ Giessen, Inst Theoret Phys 3, Heinrich Buff Ring 16, D-35392 Giessen, Germany.
   Univ Giessen, Inst Theoret Phys 3, D-35392 Giessen, Germany.
   Bar Ilan Univ, Minerva Ctr, IL-52100 Ramat Gan, Israel.
   Bar Ilan Univ, Dept Phys, IL-52100 Ramat Gan, Israel.}},
DOI = {{10.1016/S0378-4371(02)01509-1}},
Article-Number = {{PII S0378-4371(02)01509-1}},
ISSN = {{0378-4371}},
Keywords = {{phase synchronization; cross-correlation; time lag; atmosphere;
   teleconnection}},
Keywords-Plus = {{PERSISTENCE}},
Research-Areas = {{Physics}},
Web-of-Science-Categories  = {{Physics, Multidisciplinary}},
ORCID-Numbers = {{Rybski, Diego/0000-0001-6125-7705}},
Cited-References = {{BARNSTON AG, 1987, MON WEATHER REV, V115, P1083, DOI 10.1175/1520-0493(1987)115<1083:CSAPOL>2.0.CO;2.
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Number-of-Cited-References = {{11}},
Times-Cited = {{41}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{1}},
Journal-ISO = {{Physica A}},
Doc-Delivery-Number = {{652JJ}},
Unique-ID = {{ISI:000181375800050}},
DA = {{2020-08-06}},
}

@article{ ISI:000182072100009,
Author = {Wang, YF and Yasushi, F and Kuranoshin, K},
Title = {{A teleconnection pattern related with the development of the Okhotsk
   high and the northward progress of the subtropical high in East Asian
   summer}},
Journal = {{ADVANCES IN ATMOSPHERIC SCIENCES}},
Year = {{2003}},
Volume = {{20}},
Number = {{2}},
Pages = {{237-244}},
Month = {{MAR}},
Abstract = {{This study examines the relationship between the subtropical high in the
   West Pacific and the Okhotsk high in summer, and explains why the
   subtropical high cannot progress northward when the Okhotsk high is
   active. The findings are as follows. (1) A teleconnection pattern,
   namely, the significant correlation dipole between the index of the
   Okhotsk high and 500 hPa geopotential height (Z500), over East Asia,
   tends to occur in summer. (2) The teleconnection is closely related to
   the wave train propagation from the Okhotsk Sea via Japan to the
   subtropical regions when the Okhotsk high is developing. (3) The wave
   train propagation associated with the development of the Okhotsk high
   can generate a large cyclonic anomaly over the sea east of Japan, even
   in late summer. The cyclonic anomaly plays an important role in
   weakening the northern part of the subtropical high. The anomalous
   southern position of the main body of the subtropical high in the summer
   of 1998 is partly due to this effect.}},
Publisher = {{SCIENCE PRESS}},
Address = {{16 DONGHUANGCHENGGEN NORTH ST, BEIJING 100717, PEOPLES R CHINA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Wang, YF (Corresponding Author), Chinese Acad Meteorol Sci, Beijing 100081, Peoples R China.
   Chinese Acad Meteorol Sci, Beijing 100081, Peoples R China.
   Hokkaido Univ, Inst Low Temp Sci, Sapporo, Hokkaido 060, Japan.
   Okayama Univ, Fac Educ, Okayama 7008530, Japan.}},
ISSN = {{0256-1530}},
EISSN = {{1861-9533}},
Keywords = {{Okhotsk high; subtropical high; Rossby wave}},
Keywords-Plus = {{CIRCULATION; ATMOSPHERE; PACIFIC; IMPACT}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{yfwang@cams.cma.gov.cn}},
Cited-References = {{HOSKINS BJ, 1981, J ATMOS SCI, V38, P1179, DOI 10.1175/1520-0469(1981)038<1179:TSLROA>2.0.CO;2.
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   YE D, 1996, STUDY MECH DROUGHT F.
   ZHU Q, 1979, PRINCIPLE METHOD SYN.}},
Number-of-Cited-References = {{17}},
Times-Cited = {{5}},
Usage-Count-Last-180-days = {{2}},
Usage-Count-Since-2013 = {{6}},
Journal-ISO = {{Adv. Atmos. Sci.}},
Doc-Delivery-Number = {{664QQ}},
Unique-ID = {{ISI:000182072100009}},
DA = {{2020-08-06}},
}

@article{ ISI:000181537100003,
Author = {Dinc, M and Haynes, KE and Tarimcilar, M},
Title = {{Integrating models for regional development decisions: A policy
   perspective}},
Journal = {{ANNALS OF REGIONAL SCIENCE}},
Year = {{2003}},
Volume = {{37}},
Number = {{1}},
Pages = {{31-53}},
Month = {{MAR}},
Abstract = {{This paper develops and demonstrates a combined set of models to capture
   regional development decision processes. The results of the models are
   then integrated along with other socio-political factors within a policy
   relevant decision methodology framework. The Haynes and Dine (1997)
   extension of the shift-share model identifies regional industrial
   sectors for analysis based on their scale, productivity and sources of
   productivity change. By employing Data Envelopment Analysis (DEA), the
   efficiency of these lead sectors is investigated and the future
   competitiveness of these sectors is evaluated. By incorporating
   input-output analysis the impact of inter-sectoral transactions. on
   sectoral efficiency is assessed. Since in most cases state economic
   development planning and implementation processes also involve political
   judgements, based on the findings of the above models, the study
   suggests a decision support framework which combines the above mentioned
   quantitative tools with other qualitative decision factors. An
   Analytical Hierarchy Process (AHP) is employed as a multi-objective
   decision making device to integrate the relevant policy components.}},
Publisher = {{SPRINGER-VERLAG}},
Address = {{175 FIFTH AVE, NEW YORK, NY 10010 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Dinc, M (Corresponding Author), World Bank, 1818 H St NW, Washington, DC 20433 USA.
   World Bank, Washington, DC 20433 USA.
   George Mason Univ, Sch Publ Policy, Fairfax, VA 22030 USA.
   George Washington Univ, Sch Business \& Management, Washington, DC 20052 USA.}},
DOI = {{10.1007/s001680200093}},
ISSN = {{0570-1864}},
Keywords-Plus = {{DATA ENVELOPMENT ANALYSIS; EFFICIENCY; DEA}},
Research-Areas = {{Business \& Economics; Environmental Sciences \& Ecology; Geography;
   Public Administration}},
Web-of-Science-Categories  = {{Economics; Environmental Studies; Geography; Regional \& Urban Planning}},
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Number-of-Cited-References = {{48}},
Times-Cited = {{15}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{8}},
Journal-ISO = {{Ann. Reg. Sci.}},
Doc-Delivery-Number = {{655DY}},
Unique-ID = {{ISI:000181537100003}},
DA = {{2020-08-06}},
}

@article{ ISI:000180099100007,
Author = {Borges, AR and Antunes, CH},
Title = {{A fuzzy multiple objective decision support model for energy-economy
   planning}},
Journal = {{EUROPEAN JOURNAL OF OPERATIONAL RESEARCH}},
Year = {{2003}},
Volume = {{145}},
Number = {{2}},
Pages = {{304-316}},
Month = {{MAR 1}},
Abstract = {{In this paper an interactive approach to deal with fuzzy multiple
   objective linear programming problems is presented, which is based on
   the analysis of the decomposition of the parametric (weight) diagram
   into indifference regions corresponding to basic efficient solutions.
   This approach is illustrated to tackle uncertainty and imprecision
   associated with the coefficients of an input-output energy-economy
   planning model, aimed at providing decision support to decision makers
   in the study of the interactions between the energy system and the
   economy on a national level. (C) 2002 Published by Elsevier Science B.V.}},
Publisher = {{ELSEVIER SCIENCE BV}},
Address = {{PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Borges, AR (Corresponding Author), Coimbra Polytech Inst, ISEC, Apartado 10057, P-3030601 Coimbra, Portugal.
   Coimbra Polytech Inst, ISEC, P-3030601 Coimbra, Portugal.
   INESC, P-3000033 Coimbra, Portugal.
   Univ Coimbra, Dept Elect Engn, P-3030030 Coimbra, Portugal.}},
DOI = {{10.1016/S0377-2217(02)00536-2}},
Article-Number = {{PII S0377-2217(02)00536-2}},
ISSN = {{0377-2217}},
Keywords = {{fuzzy multiple objective linear programming; decision support systems;
   interactive methods; energy system; input-output analysis}},
Keywords-Plus = {{LINEAR-PROGRAMMING PROBLEMS}},
Research-Areas = {{Business \& Economics; Operations Research \& Management Science}},
Web-of-Science-Categories  = {{Management; Operations Research \& Management Science}},
Author-Email = {{arborges@isec.pt}},
ResearcherID-Numbers = {{Henggeler, Carlos/F-8517-2011
   }},
ORCID-Numbers = {{Henggeler, Carlos/0000-0003-4754-2168
   Borges, Ana Rosa Pereira/0000-0003-3167-8714}},
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Number-of-Cited-References = {{21}},
Times-Cited = {{69}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{15}},
Journal-ISO = {{Eur. J. Oper. Res.}},
Doc-Delivery-Number = {{630GL}},
Unique-ID = {{ISI:000180099100007}},
DA = {{2020-08-06}},
}

@article{ ISI:000181456400005,
Author = {Coleman, JSM and Rogers, JC},
Title = {{Ohio River Valley winter moisture conditions associated with the
   Pacific-North American teleconnection pattern}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2003}},
Volume = {{16}},
Number = {{6}},
Pages = {{969-981}},
Month = {{MAR}},
Abstract = {{The relationship between the Pacific-North American (PNA) teleconnection
   pattern and Ohio River Valley (ORV) winter precipitation and hydrology
   is described. The PNA is significantly linked to moisture variability in
   an area extending from southeastern Missouri, northeastward over states
   adjacent to the Ohio River through Ohio. Maximum correlation between the
   PNA index and station precipitation peaks in southern Indiana at r =
   -0.71, making the circulation/climate teleconnection one of the
   strongest in the Northern Hemisphere. The North Pacific index (NPI), a
   Pacific basin sea level pressure index that is highly correlated to the
   PNA, confirms a strong circulation-ORV precipitation relationship
   extending back to 1899. In contrast, measures such as the Tahiti-Darwin
   Southern Oscillation index (SOI) and Nino-3.4 (5degreesS-5degreesN,
   120degrees-170degreesW) sea temperatures are not significantly
   correlated to ORV winter precipitation. Wettest (driest) winters occur
   with zonal (meridional) flow with the PNA negative (positive) and North
   Pacific sea level pressure anomalously high (low). Moisture flux
   convergence extends much farther north from the Gulf of Mexico in the
   wet winters, compared to dry, and excess of precipitation over
   evaporation (moisture budget) is over 100 mm larger throughout much of
   the ORV. Wet winters, particularly those of 1949 and 1950 changed the
   ORV hydrology to one of extensive wet conditions, as measured by the
   Palmer hydrologic drought index (PHDI). Unusually dry winters, however,
   appear to have less impact on the index; many ORV climate divisions
   remain moist through the winter despite low precipitation. Winter mean
   streamflow along the Ohio River and its tributaries varies significantly
   between PNA extremes, with river discharges up to 100\% higher in
   PNA-negative winters as opposed to PNA-positive winters.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Coleman, JSM (Corresponding Author), Ohio State Univ, Dept Geog, 1035 Derby Hall,154 N Oval Mall, Columbus, OH 43210 USA.
   Ohio State Univ, Dept Geog, Columbus, OH 43210 USA.}},
DOI = {{10.1175/1520-0442(2003)016<0969:ORVWMC>2.0.CO;2}},
ISSN = {{0894-8755}},
Keywords-Plus = {{SURFACE TEMPERATURE ANOMALIES; UNITED-STATES; PRECIPITATION; CLIMATE;
   DROUGHT; VARIABILITY; ENSO}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Cited-References = {{COLEMAN JSM, 2000, THESIS OHIO STATE U.
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Number-of-Cited-References = {{30}},
Times-Cited = {{54}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{14}},
Journal-ISO = {{J. Clim.}},
Doc-Delivery-Number = {{653UX}},
Unique-ID = {{ISI:000181456400005}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000181094800008,
Author = {Hsieh, WW and Yuval and Li, JY and Shabbar, A and Smith, S},
Title = {{Seasonal prediction with error estimation of Columbia river streamflow
   in British Columbia}},
Journal = {{JOURNAL OF WATER RESOURCES PLANNING AND MANAGEMENT-ASCE}},
Year = {{2003}},
Volume = {{129}},
Number = {{2}},
Pages = {{146-149}},
Month = {{MAR-APR}},
Abstract = {{Large-scale climatological states {[}tropical Pacific sea surface
   temperatures (SST), Pacific-North American (PNA) atmospheric
   teleconnection and Pacific Decadal Oscillation (PDO)] and local
   precipitation data are used to predict the April-August Columbia River
   streamflow at Donald, British Columbia, Canada. Using predictors up to
   the end of November in the preceding year, forecasts of the April-August
   streamflow were made by multiple linear regression (MLR) under a
   jackknife scheme. A correlation skill of 0.52 is attained using PDO, PNA
   and SST as predictors, with PDO being the strongest and SST the weakest.
   When local precipitation is added among the predictors, PDO becomes
   redundant, and MLR with precipitation, PNA and SST as predictors
   attained a correlation skill of 0.70. Feedforward neural-network models
   were used for nonlinear regression, but the results were essentially
   identical to the MLR predictions, implying that the detectable
   relationships in the short, 49-sample record are linear. A bootstrap
   process estimates the relative errors of the MLR predictions.}},
Publisher = {{ASCE-AMER SOC CIVIL ENGINEERS}},
Address = {{1801 ALEXANDER BELL DR, RESTON, VA 20191-4400 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Hsieh, WW (Corresponding Author), Univ British Columbia, Dept Earth \& Ocean Sci, Vancouver, BC V6T 1Z4, Canada.
   Univ British Columbia, Dept Earth \& Ocean Sci, Vancouver, BC V6T 1Z4, Canada.
   Meteorol Serv Canada, Downsview, ON M3H 5T4, Canada.}},
DOI = {{10.1061/(ASCE)0733-9496(2003)129:2(146)}},
ISSN = {{0733-9496}},
Keywords = {{Canada; stream flow; seasonal variations; errors; prediction}},
Keywords-Plus = {{WESTERN UNITED-STATES; VARIABILITY; CLIMATE; ENSO}},
Research-Areas = {{Engineering; Water Resources}},
Web-of-Science-Categories  = {{Engineering, Civil; Water Resources}},
ResearcherID-Numbers = {{Hsieh, William W/G-8380-2011}},
ORCID-Numbers = {{Hsieh, William W/0000-0003-2654-392X}},
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Number-of-Cited-References = {{13}},
Times-Cited = {{22}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{3}},
Journal-ISO = {{J. Water Resour. Plan. Manage.-ASCE}},
Doc-Delivery-Number = {{647LT}},
Unique-ID = {{ISI:000181094800008}},
DA = {{2020-08-06}},
}

@article{ ISI:000187026100002,
Author = {Hardy, JW and Henderson, KG},
Title = {{Cold front variability in the southern United States and the influence
   of atmospheric teleconnection patterns}},
Journal = {{PHYSICAL GEOGRAPHY}},
Year = {{2003}},
Volume = {{24}},
Number = {{2}},
Pages = {{120-137}},
Month = {{MAR-APR}},
Abstract = {{The variability of cold front passages in the southern United States and
   the effects of three teleconnection patterns on cold front frequencies
   are analyzed in this study. The Southern Oscillation is weakly
   correlated with cold front frequencies. However, cold front passage
   frequencies during El Nino and La Nina events are not significantly
   different. The Pacific/North American (PNA) and North Atlantic
   Oscillation (NAO) teleconnection patterns exert a significant influence
   on cold front variability in this region. The PNA pattern is most
   strongly tied to variations in cold front passage frequencies in
   Florida. Meridional (zonal) flow conditions are associated with a
   southward (northward) displacement of storm tracks over the eastern
   United States, resulting in an increase (decrease) in cold front
   passages in Florida. Various parts of the southern United States are
   affected by the NAO. High NAO months are characterized by an expanded
   Atlantic Subtropical High which often results in fewer cold front
   passages in the eastern portions of the southern United States. During
   low NAO months, much of Texas experiences a higher frequency of cold
   front passages, a likely result of increased upper-air trough
   development over the region.}},
Publisher = {{V H WINSTON \& SON INC}},
Address = {{360 SOUTH OCEAN BLVD, PH-B, PALM BEACH, FL 33480 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Hardy, JW (Corresponding Author), E Stroudsburg Univ, Dept Geog, E Stroudsburg, PA 18301 USA.
   E Stroudsburg Univ, Dept Geog, E Stroudsburg, PA 18301 USA.
   Villanova Univ, Dept Geog, Villanova, PA 19085 USA.}},
DOI = {{10.2747/0272-3646.24.2.120}},
ISSN = {{0272-3646}},
Keywords = {{cold fronts; teleconnections; southern United States}},
Keywords-Plus = {{NORTHERN-HEMISPHERE WINTER; CITRUS FREEZES; OSCILLATION; FREQUENCY;
   MEXICO; GULF; ASSOCIATIONS; RAINFALL; CLIMATE; EUROPE}},
Research-Areas = {{Environmental Sciences \& Ecology; Physical Geography; Geology;
   Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Environmental Sciences; Geography, Physical; Geosciences,
   Multidisciplinary; Meteorology \& Atmospheric Sciences}},
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