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Number-of-Cited-References = {{24}},
Times-Cited = {{1}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{2}},
Journal-ISO = {{Int. J. Climatol.}},
Doc-Delivery-Number = {{830FC}},
Unique-ID = {{ISI:000222106100004}},
DA = {{2020-08-06}},
}

@article{ ISI:000223303800004,
Author = {Zhang, ML and Cheng, H and Yuan, DX and Lin, YS and Qin, JM and Wang, H
   and Feng, YM and Tu, LL and Zhang, HL},
Title = {{High-resolution climate records from two stalagmites in Qixin Cave,
   southern Guizhou, and Heinrich events during the last glacial period}},
Journal = {{EPISODES}},
Year = {{2004}},
Volume = {{27}},
Number = {{2}},
Pages = {{112-118}},
Month = {{JUN}},
Abstract = {{The time sequence of high-resolution paleoclimatic changes since the
   last glacial period-60,500 yr B.P.- has been reconstructed with
   high-precision TIMS-U series dates and analyses of the oxygen isotopes
   from Q4 and Q6 stalagmites of the Qixin Cave in southern Guizhou.
   Comparative analyses of delta(18)O curves from the GISP2' ice core and
   the two stalagmites shows that the depositional records of the
   Dansgaard-Oeschger cycle events 1-18 and Heinrich's events H1-H5 from
   the records of the two stalagmites reflect rapid climate changes over a
   short time scale since the last glacial stage, and indicates the precise
   boundary lines at which the cold events occurred. The study results have
   shown that the records of the cold and warm events from the two
   stalagmites since 60,500 yr B.P. are the reflection of the paleo-monsoon
   circulation. Changes are clearly affected by the climate oscillation of
   the North Atlantic Ocean, and indicate that they have a strong
   teleconnection with the paleoclimate changes that occurred in the North
   Polar region.
   The records of delta(18)O from the Q4 and Q6 stalagmites indicate that
   the delta(18)O values from 60,590 yr B.P, to 11,290 yr B.P. changed from
   a more negative (or lighter) drift to a heavier or positive drift trend
   in the last glacial period. The data reflect the weakening of the Asian
   summer monsoon and the climate which generally became drier and cooler.}},
Publisher = {{GEOLOGICAL SOC KOREA}},
Address = {{KOREA SCIENCE \& TECHNOLOGY CTR, RM 813, 7 GIL 22, TEHERAN- RO,
   GANGNAM-GUNA, SEOUL, 06130, SOUTH KOREA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Zhang, ML (Corresponding Author), CAGS, Inst Karst Geol, Karst Dynam Lab, Guilin 541004, Peoples R China.
   CAGS, Inst Karst Geol, Karst Dynam Lab, Guilin 541004, Peoples R China.
   Univ Minnesota, Dept Geol \& Geophys, Minneapolis, MN 55455 USA.}},
ISSN = {{0705-3797}},
Keywords-Plus = {{NORTH-ATLANTIC; YOUNGER DRYAS; SULU-SEA; OXYGEN; ICE; INSTABILITY;
   DISCHARGES; OCEAN}},
Research-Areas = {{Geology}},
Web-of-Science-Categories  = {{Geosciences, Multidisciplinary}},
Author-Email = {{mlzh@karst.edu.cn}},
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Number-of-Cited-References = {{26}},
Times-Cited = {{10}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{7}},
Journal-ISO = {{Episodes}},
Doc-Delivery-Number = {{846GN}},
Unique-ID = {{ISI:000223303800004}},
DA = {{2020-08-06}},
}

@article{ ISI:000221849500016,
Author = {Ortiz, JD and O'Connell, SB and DelViscio, J and Dean, W and Carriquiry,
   JD and Marchitto, T and Zheng, Y and van Geen, A},
Title = {{Enhanced marine productivity off western North America during warm
   climate intervals of the past 52 ky}},
Journal = {{GEOLOGY}},
Year = {{2004}},
Volume = {{32}},
Number = {{6}},
Pages = {{521-524}},
Month = {{JUN}},
Abstract = {{Studies of the Santa Barbara Basin off the coast of California have
   linked changes in its bottom-water oxygen content to millennial-scale
   climate changes as recorded by the oxygen isotope composition of
   Greenland ice. Through the use of detailed records from a sediment core
   collected off the Magdalena Margin of Baja California, Mexico, we
   demonstrate that this teleconnection predominantly arose from changes in
   marine productivity, rather than changes in ventilation of the North
   Pacific, as was originally proposed. One possible interpretation is that
   the modern balance of El Nino-La Nina conditions that favors a shallow
   nutricline and high productivity today and during warm climate intervals
   of the past 52 k.y. was altered toward more frequent, deep nutricline,
   low productivity, El Nino-like conditions during cool climate intervals.}},
Publisher = {{GEOLOGICAL SOC AMER, INC}},
Address = {{PO BOX 9140, BOULDER, CO 80301-9140 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Ortiz, JD (Corresponding Author), Columbia Univ, Lamont Doherty Geol Observ, Palisades, NY 10964 USA.
   Columbia Univ, Lamont Doherty Geol Observ, Palisades, NY 10964 USA.
   Kent State Univ, Dept Geol, Kent, OH 44242 USA.
   Wesleyan Univ, Dept Earth \& Environm Sci, Middletown, CT 06459 USA.
   US Geol Survey, Earth Surface Proc, Lakewood, CO 80225 USA.
   Univ Autonoma Baja California, Inst Invest Oceanol, Ensenada, Baja California, Mexico.
   Univ Colorado, Inst Arctic \& Alpine Res, Boulder, CO 80309 USA.
   Univ Colorado, Dept Geol Sci, Boulder, CO 80309 USA.
   CUNY Queens Coll, Sch Earth \& Environm Sci, Flushing, NY 11367 USA.}},
DOI = {{10.1130/G20234.1}},
ISSN = {{0091-7613}},
EISSN = {{1943-2682}},
Keywords = {{millennial-scale climate; abrupt climate change; foraminifera; marine
   productivity; paleo-ENSO variability}},
Keywords-Plus = {{SANTA-BARBARA BASIN; CALIFORNIA CURRENT SYSTEM; OXYGEN-MINIMUM ZONE;
   NITROGEN ISOTOPE; EL-NINO; PACIFIC; OCEAN; SEDIMENTATION; SURFACE;
   WATERS}},
Research-Areas = {{Geology}},
Web-of-Science-Categories  = {{Geology}},
Author-Email = {{avangeen@ldeo.columbia.edu}},
ResearcherID-Numbers = {{Ortiz, Joseph/E-1144-2011
   CARRIQUIRY, JOSE/R-9190-2017
   HUANG, Feiyan/G-5182-2018
   }},
ORCID-Numbers = {{Ortiz, Joseph/0000-0002-6583-3850
   HUANG, Feiyan/0000-0003-4846-7913
   ZHENG, Yan/0000-0001-5256-9395}},
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Number-of-Cited-References = {{31}},
Times-Cited = {{88}},
Usage-Count-Last-180-days = {{3}},
Usage-Count-Since-2013 = {{20}},
Journal-ISO = {{Geology}},
Doc-Delivery-Number = {{826SS}},
Unique-ID = {{ISI:000221849500016}},
DA = {{2020-08-06}},
}

@article{ ISI:000221451200012,
Author = {Ortega, M and Lin, L},
Title = {{Control theory applications to the production-inventory problem: a
   review}},
Journal = {{INTERNATIONAL JOURNAL OF PRODUCTION RESEARCH}},
Year = {{2004}},
Volume = {{42}},
Number = {{11}},
Pages = {{2303-2322}},
Month = {{JUN 1}},
Abstract = {{Mathematical models based on average or steady-state conditions are
   insufficient when dealing with dynamic situations faced by
   production-inventory systems in current business environments.
   Therefore, the use of mathematical tools based on control theory to
   handle time-varying phenomena has been reinvigorated in order to
   accommodate these new needs. Given the variety of research approaches in
   the field over several decades, there is a need to provide a review of
   this work. This review identifies some major research efforts for
   applying control theoretic methods to production-inventory systems. It
   is shown that in general, control theory is applied to reduce inventory
   variation, reduce demand amplification and optimize ordering rules. Some
   control theory tools applied are block diagram algebra, Mason's gain
   formula, Bode plots, Laplace transform, Z transform and optimal control.
   Basic approaches are classified within stochastic control theory and
   deterministic control theory. Two important issues are then identified
   within the deterministic models. First, separate efforts to integrate
   systems horizontally (i.e. supply chain) or vertically (i.e.
   hierarchical approach) are identified. Second, none of the reviewed
   models implemented a systematic way to calculate all the required model
   parameters. Some authors presented suggestions to optimize some
   parameters, but no reference was found that tried to obtain these
   parameter values from a real system.}},
Publisher = {{TAYLOR \& FRANCIS LTD}},
Address = {{4 PARK SQUARE, MILTON PARK, ABINGDON OX14 4RN, OXON, ENGLAND}},
Type = {{Review}},
Language = {{English}},
Affiliation = {{Ortega, M (Corresponding Author), Tech Inst Chihuahua 2, Dept Ind Engn, MBE 38-53,220 Basset Ave, El Paso, TX 79901 USA.
   Tech Inst Chihuahua 2, Dept Ind Engn, El Paso, TX 79901 USA.}},
DOI = {{10.1080/00207540410001666260}},
ISSN = {{0020-7543}},
Keywords-Plus = {{INPUT-OUTPUT-ANALYSIS; FLEXIBLE MANUFACTURING SYSTEMS; SUPPLY CHAIN;
   CONTROL POLICIES; DYNAMIC ANALYSIS; SAFETY STOCKS; DESIGN; PERFORMANCE;
   SIMULATION; MANAGEMENT}},
Research-Areas = {{Engineering; Operations Research \& Management Science}},
Web-of-Science-Categories  = {{Engineering, Industrial; Engineering, Manufacturing; Operations Research
   \& Management Science}},
Author-Email = {{maximo\_ortega@hotmail.com}},
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Number-of-Cited-References = {{63}},
Times-Cited = {{116}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{45}},
Journal-ISO = {{Int. J. Prod. Res.}},
Doc-Delivery-Number = {{821HO}},
Unique-ID = {{ISI:000221451200012}},
DA = {{2020-08-06}},
}

@article{ ISI:000221758000001,
Author = {Saenko, OA and Schmittner, A and Weaver, AJ},
Title = {{The Atlantic-Pacific seesaw}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2004}},
Volume = {{17}},
Number = {{11}},
Pages = {{2033-2038}},
Month = {{JUN}},
Abstract = {{A global, oceanic teleconnection of salinity, meridional overturning
   circulation (MOC), and climate of the North Atlantic and North Pacific
   is proposed. Simulations with a global climate model show that an
   extraction of freshwater from the Pacific results not only in an
   increase of salinity there, but also in a decrease of salinity in the
   Atlantic. As a result, a Pacific MOC develops while the Atlantic MOC
   collapses without freshwater perturbation in the Atlantic. Similarly, an
   input of freshwater to the Atlantic leads not only to a decrease of
   salinity there, but also to an increase of salinity in the Pacific. The
   Atlantic MOC collapses, whereas the Pacific MOC develops without
   freshwater perturbation in the Pacific. The mechanism behind this
   antiphase Atlantic Pacific relationship is the positive feedback between
   ocean circulation and salinity contrasts, originally proposed by Stommel
   to operate between low and high latitudes. Here the authors show that
   the same mechanism operates on the Atlantic-Pacific interbasin scale,
   with the Southern Ocean acting as a pivot point for the interbasin
   seesaw. The proposed Atlantic-Pacific seesaw effect helps to explain
   some major out-of-phase oscillations of the climate states between the
   North Atlantic and North Pacific during the last deglaciation.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Saenko, OA (Corresponding Author), Univ Victoria, Meteorol Serv Canada, Canadian Ctr Climate Modelling \& Anal, POB 1700, Victoria, BC V8W 2Y2, Canada.
   Univ Victoria, Meteorol Serv Canada, Canadian Ctr Climate Modelling \& Anal, Victoria, BC V8W 2Y2, Canada.
   Univ Kiel, Inst Geowissensch, Kiel, Germany.
   Univ Victoria, Sch Earth \& Ocean Sci, Victoria, BC, Canada.}},
DOI = {{10.1175/1520-0442(2004)017<2033:TAS>2.0.CO;2}},
ISSN = {{0894-8755}},
Keywords-Plus = {{OCEAN THERMOHALINE CIRCULATION; NORTH PACIFIC; MODEL}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{oleg.saenko@ec.gc.ca}},
ResearcherID-Numbers = {{Schmittner, Andreas/A-3101-2008
   Schmittner, Andreas/O-9647-2015
   Weaver, Andrew J/E-7590-2011}},
ORCID-Numbers = {{Schmittner, Andreas/0000-0002-8376-0843
   Weaver, Andrew J/0000-0001-8919-3598}},
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Number-of-Cited-References = {{14}},
Times-Cited = {{80}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{7}},
Journal-ISO = {{J. Clim.}},
Doc-Delivery-Number = {{825LB}},
Unique-ID = {{ISI:000221758000001}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000223245100001,
Author = {Lang, TJ and Barros, AP},
Title = {{Winter storms in the central Himalayas}},
Journal = {{JOURNAL OF THE METEOROLOGICAL SOCIETY OF JAPAN}},
Year = {{2004}},
Volume = {{82}},
Number = {{3}},
Pages = {{829-844}},
Month = {{JUN}},
Abstract = {{Based on observations from a hydrometeorological network on the eastern
   slopes of the Annapurna Range, nearly all the annual precipitation at
   low elevations (< 2000 in MSL) in Nepal is in liquid form, even during
   the winter. However, high elevations (> 3000 in MSL) can receive up to
   40\% of their annual precipitation as snowfall during the winter, with
   the highest altitude stations (similar to4000 in MSL and above) having
   the most total winter precipitation (which can exceed 100 cm).
   Significant snowstorms are associated with terrain-locked low-pressure
   systems that form when an upper-level disturbance passes over the notch
   formed by the Himalayas and Hindu Kush mountains (the so-called Western
   Disturbances), causing upper-level SW flow over central Nepal and
   orographically forced precipitation. Based on these results, a 30-year
   (1973-2002) climatology of these notch depressions is developed and
   reveals that significant interannual variability in central Himalayan
   winter storms exists. Weak but statistically significant correlation
   between notch depressions and the Polar/Eurasia teleconnection pattern
   was found, suggesting that the strength of the circumpolar vortex may
   affect the number of depressions passing through the Himalayan region. A
   typical snow event (11 February 2000) was the subject of an
   observational and modeling case study. Local precipitation (snow and
   rain) and other meteorological observations, as well as satellite
   (Meteosat-5 and TRMM) and NCEP/NCAR Reanalysis data were used, along
   with a cloud-resolving model with realistic topography. This study shows
   that significant wintertime precipitation only occurs in the central
   Himalayas when the large-scale flow evolves to a favorable geometry with
   respect to the mountains.}},
Publisher = {{METEOROLOGICAL SOC JAPAN}},
Address = {{C/O JAPAN METEOROLOGICAL AGENCY 1-3-4 OTE-MACHI, CHIYODA-KU, TOKYO,
   100-0004, JAPAN}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Barros, AP (Corresponding Author), Duke Univ, Dept Civil \& Environm Engn, Pratt Sch Engn, 121 Hudson Hall,Box 90287, Durham, NC 27708 USA.
   Harvard Univ, Div Engn \& Appl Sci, Cambridge, MA 02138 USA.}},
DOI = {{10.2151/jmsj.2004.829}},
ISSN = {{0026-1165}},
EISSN = {{2186-9057}},
Keywords-Plus = {{INDIAN MONSOON RAINFALL; ADVECTION TRANSPORT ALGORITHM; EURASIAN SNOW
   COVER; SUMMER MONSOON; CENTRAL NEPAL; INTERANNUAL VARIABILITY; APPARENT
   RELATIONSHIP; THERMAL CONTRAST; SIMULATIONS; PRECIPITATION}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{ana.barros@duke.edu}},
ResearcherID-Numbers = {{Barros, Ana P/A-3562-2011
   }},
ORCID-Numbers = {{Barros, Ana P/0000-0003-4606-3106
   Lang, Timothy/0000-0003-1576-572X}},
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   UENO K, 2001, B GLACIOL RES, V18, P23.}},
Number-of-Cited-References = {{28}},
Times-Cited = {{126}},
Usage-Count-Last-180-days = {{2}},
Usage-Count-Since-2013 = {{15}},
Journal-ISO = {{J. Meteorol. Soc. Jpn.}},
Doc-Delivery-Number = {{845LV}},
Unique-ID = {{ISI:000223245100001}},
OA = {{Bronze, Green Published}},
DA = {{2020-08-06}},
}

@article{ ISI:000221746100001,
Author = {Faerge, J and Magid, J},
Title = {{Evaluating NUTMON nutrient balancing in Sub-Saharan Africa}},
Journal = {{NUTRIENT CYCLING IN AGROECOSYSTEMS}},
Year = {{2004}},
Volume = {{69}},
Number = {{2}},
Pages = {{101-110}},
Month = {{JUN}},
Abstract = {{Nutrient balances for the last two decades in Sub-Saharan Africa (SSA)
   reveal, almost unequivocally, alarming nutrient deficiencies. The
   nutrient balancing in SSA was initiated by Stoorvogel and Smaling
   {[}Report 28, Winand Staring Centre, 1990] and Smaling et al. {[}Fert.
   Res. 35 (2003) 237]. Their nutrient monitoring (NUTMON) concept is
   conducted as input-output analysis. Inputs are fertilizers, mineral and
   organic, wet and dry deposition, nitrogen fixation and sedimentation.
   Outputs are harvested crops and residues, leaching, denitrification and
   erosion. Nutrient flows, as fertilizers and harvested crops, are in
   general measured or estimated by interviews, whereas flows that are
   difficult to quantify, such as leaching, denitrification and erosion,
   are modeled by means of transfer functions mainly elaborated by the
   NUTMON initiators. Generally, for the NUTMON studies the average losses
   worked out by means of transfer functions seem high in comparison to
   similar rates in high input agriculture in temperate regions. Therefore,
   we decided to review some of the original transfer functions and their
   impact on the NUTMON calculations. The review revealed that the transfer
   functions have a strong tendency to overestimate losses. No attempts
   have been made to validate whether the modeled losses are consistent to
   empirical measurements for the actual locations for which the nutrient
   balances have been applied. Contemporary NUTMON studies rely on the
   original transfer functions, as well as the original assumptions
   employed in the parameterisation. Therefore, NUTMON balances are bound
   to reveal alarming nutrient deficiencies, no matter what the SSA farmers
   do.}},
Publisher = {{SPRINGER}},
Address = {{VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Faerge, J (Corresponding Author), Jenslevvej 69, DK-4070 Kirke Hyllinge, Denmark.
   Royal Vet \& Agr Univ, Plant Nutr \& Soil Fertil Lab, DK-1871 Frederiksberg, Denmark.}},
DOI = {{10.1023/B:FRES.0000029680.97610.51}},
ISSN = {{1385-1314}},
EISSN = {{1573-0867}},
Keywords = {{N leaching; NUTMON; nutrient balancing; Sub-Saharan Africa; transfer
   functions}},
Keywords-Plus = {{FARMING SYSTEMS NUTMON; ECONOMIC-PERFORMANCE; NITROGEN; FLOWS;
   DENITRIFICATION; DEPLETION; DYNAMICS; DISTRICT; ETHIOPIA; LOSSES}},
Research-Areas = {{Agriculture}},
Web-of-Science-Categories  = {{Soil Science}},
Author-Email = {{jensfaerge@hotmail.com}},
ResearcherID-Numbers = {{Magid, Jakob/C-4558-2013}},
ORCID-Numbers = {{Magid, Jakob/0000-0001-5867-0910}},
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Number-of-Cited-References = {{55}},
Times-Cited = {{28}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{11}},
Journal-ISO = {{Nutr. Cycl. Agroecosyst.}},
Doc-Delivery-Number = {{825HE}},
Unique-ID = {{ISI:000221746100001}},
DA = {{2020-08-06}},
}

@article{ ISI:000223795000003,
Author = {Rogers, JC and Coleman, JSM},
Title = {{Ohio winter precipitation and stream flow associations to Pacific
   atmospheric and oceanic teleconnection patterns}},
Journal = {{OHIO JOURNAL OF SCIENCE}},
Year = {{2004}},
Volume = {{104}},
Number = {{3}},
Pages = {{51-59}},
Month = {{JUN}},
Abstract = {{The relationship between the Pacific/North American (PNA) atmospheric
   circulation tele-connection, equatorial Pacific sea surface temperature
   anomalies (SSTAs), and Ohio winter (DJF) precipitation and stream flow
   is described using data for 84 statewide climate stations and 29 rivers.
   Maximum correlations between the PNA index (PNAI) and station
   precipitation reach r = -0.7 in southwestern Ohio (n = 53) and are as
   high as r = +0.6 (n = 104) using a proxy North Pacific index (NPI)
   comprised of sea level pressures. The Ohio winter precipitation and
   streamflow relationship with the PNAI and NPI is strongest in southern
   and southwestern Ohio, generally decreasing to non-significance over
   northern Ohio, and particularly the northeastern snow belt. In contrast,
   Nino 3.4 equatorial Pacific correlations reach r = 0.5 when SSTs precede
   winter by one month. Wettest (driest) Ohio winters occur during
   relatively zonal (meridional) flow, representing PNAI negative
   (positive) modes when north Pacific sea level pressure is anomalously
   high (low). Wet winters are characterized by a 500 hPa trough across the
   central US east of the Rockies, with surface cyclones and associated
   frontal activity traversing Ohio after originating in areas such as
   Colorado and the western Gulf of Mexico. When the meridional flow of the
   PNA positive mode occurs, Ohio winters are consistently drier than
   normal and stream flow is typically about 50\% of the PNA wet winters.
   Much higher variability occurs during PNA negative mode winters;
   precipitation and stream flow are occasionally below normal, but more
   typically above normal with some extraordinarily wet winters.}},
Publisher = {{OHIO ACAD SCIENCE}},
Address = {{1500 W 3RD AVE SUITE 223, COLUMBUS, OH 43212-2817 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Rogers, JC (Corresponding Author), Ohio State Univ, Dept Geog, Columbus, OH 43210 USA.
   Ohio State Univ, Dept Geog, Columbus, OH 43210 USA.}},
ISSN = {{0030-0950}},
Keywords-Plus = {{SURFACE TEMPERATURE ANOMALIES; NORTH-AMERICAN PRECIPITATION;
   UNITED-STATES; EL-NINO; RAINFALL; OSCILLATION; US}},
Research-Areas = {{Environmental Sciences \& Ecology; Zoology}},
Web-of-Science-Categories  = {{Ecology; Zoology}},
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Number-of-Cited-References = {{16}},
Times-Cited = {{7}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{2}},
Journal-ISO = {{Ohio J. Sci.}},
Doc-Delivery-Number = {{852ZH}},
Unique-ID = {{ISI:000223795000003}},
DA = {{2020-08-06}},
}

@article{ ISI:000221821800002,
Author = {Dwyer, L and Forsyth, P and Spurr, R},
Title = {{Evaluating tourism's economic effects: new and old approaches}},
Journal = {{TOURISM MANAGEMENT}},
Year = {{2004}},
Volume = {{25}},
Number = {{3}},
Pages = {{307-317}},
Month = {{JUN}},
Note = {{CRC Tourism Economics Workshop, Sydney, AUSTRALIA, APR, 2002}},
Abstract = {{Techniques such as multiplier analysis and Input-Output analysis are
   still very commonly used to make estimates of the economic impact of
   changes in tourism expenditure. These techniques have serious
   limitations, and as a result, alternative techniques have been developed
   to address the problems. Computable General Equilibrium (CGE) models are
   now extensively used, especially in Australia, the UK, the US and
   Canada, to estimate economic impacts of a wide variety of changes and
   policies, across most sectors. CGE techniques have been used in the
   tourism context, but so far, not extensively. Economic evaluation in
   tourism thus fails to achieve best practice. The paper presents
   arguments in support of CGE modelling as the preferred technique in
   analysing the economic impacts of tourism, and discusses its potential
   to drive future research in this area that is more relevant to real
   world tourism destinations. (C) 2003 Elsevier Ltd. All rights reserved.}},
Publisher = {{ELSEVIER SCI LTD}},
Address = {{THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND}},
Type = {{Article; Proceedings Paper}},
Language = {{English}},
Affiliation = {{Dwyer, L (Corresponding Author), Univ New S Wales, Ctr Tourism Policy Studies, Sydney, NSW 2052, Australia.
   Univ New S Wales, Ctr Tourism Policy Studies, Sydney, NSW 2052, Australia.
   Monash Univ, Dept Econ, Clayton, Vic 3800, Australia.}},
DOI = {{10.1016/S0261-5177(03)00131-6}},
ISSN = {{0261-5177}},
Keywords = {{computable general equilibrium model; input-output; economic impacts;
   tourism}},
Research-Areas = {{Environmental Sciences \& Ecology; Social Sciences - Other Topics;
   Business \& Economics}},
Web-of-Science-Categories  = {{Environmental Studies; Hospitality, Leisure, Sport \& Tourism;
   Management}},
Author-Email = {{l.dwyer@unsw.edu.au
   peter.forsyth@buseco.monash.edu.au
   r.spurr@unsw.edu.au}},
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Number-of-Cited-References = {{56}},
Times-Cited = {{294}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{52}},
Journal-ISO = {{Tourism Manage.}},
Doc-Delivery-Number = {{826IC}},
Unique-ID = {{ISI:000221821800002}},
DA = {{2020-08-06}},
}

@article{ ISI:000221610100001,
Author = {Fan, K and Wang, HJ},
Title = {{Antarctic oscillation and the dust weather frequency in North China}},
Journal = {{GEOPHYSICAL RESEARCH LETTERS}},
Year = {{2004}},
Volume = {{31}},
Number = {{10}},
Month = {{MAY 18}},
Abstract = {{The linkage between the Antarctic Oscillation (AAO) to the dust weather
   frequency (DWF) in North China is addressed. Here DWF denotes the number
   of days of dust weather events including dust haze, blowing dust and
   dust storm in one year. It is found that the interannual variation of
   AAO plays a significant role in the dust-related atmospheric circulation
   during boreal spring. AAO and DWF correlate well, with positive AAO
   tending to decrease DWF in North China. Two possible mechanisms for the
   AAO-DWF coupling are identified, one is related to a meridional
   teleconnection pattern; the other is related to a regional circulation
   pattern over the Pacific Ocean.}},
Publisher = {{AMER GEOPHYSICAL UNION}},
Address = {{2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Fan, K (Corresponding Author), Chinese Acad Sci, Nansen Zhu Int Res Ctr, Inst Atmospher Phys, 40 Huayanli, Beijing 100029, Peoples R China.
   Chinese Acad Sci, Nansen Zhu Int Res Ctr, Inst Atmospher Phys, Beijing 100029, Peoples R China.
   Yunnan Univ, Dept Atmospher Sci, Kunming 650091, Peoples R China.}},
DOI = {{10.1029/2004GL019465}},
Article-Number = {{L10201}},
ISSN = {{0094-8276}},
EISSN = {{1944-8007}},
Keywords-Plus = {{TEMPORAL VARIABILITY; APRIL 1998; TRANSPORT; STORM; PACIFIC; EVENT; ASIA}},
Research-Areas = {{Geology}},
Web-of-Science-Categories  = {{Geosciences, Multidisciplinary}},
Author-Email = {{fanke@mali.iap.ac.cn
   wanghj@mail.iap.ac.cn}},
ResearcherID-Numbers = {{Fan, Ke/AAJ-2315-2020}},
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Number-of-Cited-References = {{21}},
Times-Cited = {{138}},
Usage-Count-Last-180-days = {{3}},
Usage-Count-Since-2013 = {{33}},
Journal-ISO = {{Geophys. Res. Lett.}},
Doc-Delivery-Number = {{823KH}},
Unique-ID = {{ISI:000221610100001}},
OA = {{Green Published}},
DA = {{2020-08-06}},
}

@article{ ISI:000221949600003,
Author = {Rutllant, JA and Rosenbluth, B and Hormazabal, S},
Title = {{Intraseasonal variability of wind-forced coastal upwelling off central
   Chile (30 degrees S)}},
Journal = {{CONTINENTAL SHELF RESEARCH}},
Year = {{2004}},
Volume = {{24}},
Number = {{7-8}},
Pages = {{789-804}},
Month = {{MAY}},
Abstract = {{Satellite-derived along-shore windstress variability off subtropical
   Chile at intraseasonal periods has been recently associated with the
   corresponding wind variability over the tropical Pacific. Along the
   coastal strip in which satellite winds can not be resolved, wind-driven
   upwelling might be in principle modulated through large-scale
   intraseasonal changes in the strength of the subtropical anticyclone and
   by intraseasonal ocean coastal-trapped waves (CTWs) through associated
   changes in coastal sea-surface temperatures.
   Daily anomalies of band-passed outgoing long-wave radiation over the
   central equatorial Pacific have been selected to represent Madden-Julian
   Oscillations, as the dominant mode of equatorially sourced,
   intraseasonal variability in the atmosphere and coastal ocean. Afternoon
   alongshore pseudo-wind stresses at a representative coastal site in
   central Chile (30degreesS) describe the upwelling-favourable wind field
   over a 30-40 km coastal strip. The subtropical anticyclone strength is
   expressed as a 900-km offshore sea-level pressure (San Felix Island),
   and the sea-level pressure difference with the coast. CTWs are
   represented by the smoothed sea-level at 27degreesS.
   The intermittent nature of intraseasonal variability led to statistical
   procedures as Wavelet and Singular-Spectrum (SSA) analyses to search for
   associations among those series. Cross-correlation analysis of the
   SSA-reconstructed series with the two principal oscillatory modes
   (40-100-day, and 28-50-day periods, respectively), shows that
   intraseasonal variability in the subtropical anticyclone strength,
   partially associated with the Pacific South America teleconnection
   pattern, has the best association with coastal windstress variability.
   CTWs appeared to be important in their association with coastal winds
   only during strong MJO activity in connection with El Nino in the
   low-frequency intraseasonal band. while in the high-frequency one a
   fraction of the ASL variability appears to be locally wind-forced. (C)
   2004 Elsevier Ltd. All rights reserved.}},
Publisher = {{PERGAMON-ELSEVIER SCIENCE LTD}},
Address = {{THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Rutllant, JA (Corresponding Author), Univ Chile, Dept Geol \& Geophys, Santiago 2777, Chile.
   Univ Chile, Dept Geol \& Geophys, Santiago 2777, Chile.
   Univ Concepcion, Dept Fis Atmosfera \& Oceano, Concepcion, Chile.
   Univ Concepcion, Programa Reg Oceanog \& Clima, Concepcion, Chile.}},
DOI = {{10.1016/j.csr.2004.02.004}},
ISSN = {{0278-4343}},
Keywords = {{Humboldt current.system; coastal upwelling; local wind forcing;
   intraseasonal variability; central Chile (30 degrees S)}},
Keywords-Plus = {{MADDEN-JULIAN OSCILLATION; TEMPERATURE; PACIFIC; CIRCULATION; RAINFALL;
   SYSTEM; WAVES; MODES; ENSO}},
Research-Areas = {{Oceanography}},
Web-of-Science-Categories  = {{Oceanography}},
Author-Email = {{jrutllan@dgf.uchile.cl}},
ORCID-Numbers = {{Hormazabal, Samuel/0000-0003-0019-5058}},
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Number-of-Cited-References = {{34}},
Times-Cited = {{25}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{12}},
Journal-ISO = {{Cont. Shelf Res.}},
Doc-Delivery-Number = {{828CF}},
Unique-ID = {{ISI:000221949600003}},
DA = {{2020-08-06}},
}

@article{ ISI:000221421600011,
Author = {Schongart, J and Junk, WJ and Piedade, MTF and Ayres, JM and Huttermann,
   A and Worbes, M},
Title = {{Teleconnection between tree growth in the Amazonian floodplains and the
   El Nino-Southern Oscillation effect}},
Journal = {{GLOBAL CHANGE BIOLOGY}},
Year = {{2004}},
Volume = {{10}},
Number = {{5}},
Pages = {{683-692}},
Month = {{MAY}},
Abstract = {{There is a limited knowledge about the El Nino-Southern Oscillation
   (ENSO) effects on the Amazon basin, the world's largest tropical rain
   forest and a major factor in the global carbon cycle. Seasonal
   precipitation in the Andean watershed annually causes a several
   month-long inundation of the floodplains along the Amazon River that
   induces the formation of annual rings in trees of the flooded forests.
   Radial growth of trees is mainly restricted to the nonflooded period and
   thus the ring width corresponds to its duration. This allows the
   construction of a tree-ring chronology of the long-living hardwood
   species Piranhea trifoliata Baill. (Euphorbiaceae). El Nino causes
   anomalously low precipitation in the catchment that results in a
   significantly lower water discharge of the Amazon River and consequently
   in an extension of the vegetation period. In those years tree rings are
   significantly wider. Thus the tree-ring record can be considered as a
   robust indicator reflecting the mean climate conditions of the whole
   Western Amazon basin. We present a more than 200-year long chronology,
   which is the first ENSO-sensitive dendroclimatic proxy of the Amazon
   basin and permits the dating of preinstrumental El Nino events. Time
   series analyses of our data indicate that during the last two centuries
   the severity of El Nino increased significantly.}},
Publisher = {{WILEY}},
Address = {{111 RIVER ST, HOBOKEN 07030-5774, NJ USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Worbes, M (Corresponding Author), Univ Gottingen, Inst Agron Trop, Grisebachstr 6, D-37077 Gottingen, Germany.
   Univ Gottingen, Inst Agron Trop, D-37077 Gottingen, Germany.
   Max Planck Inst Limnol, D-24302 Plon, Germany.
   INPA, BR-69011970 Manaus, Amazonas, Brazil.
   Inst Desenvolviemto Sustentavel Mamiraua, BR-69470000 Tefe, Amazonas, Brazil.
   Univ Gottingen, Inst Forest Bot, D-37077 Gottingen, Germany.}},
DOI = {{10.1111/j.1529-8817.2003.00754.x}},
ISSN = {{1354-1013}},
EISSN = {{1365-2486}},
Keywords = {{Amazon; annual tree rings; dendrochronology; El Nino-Southern
   Oscillation; floodplain forest; paleoclimatology}},
Keywords-Plus = {{SEA-SURFACE TEMPERATURE; CLIMATE VARIABILITY; TROPICAL TREES; RINGS;
   FOREST; PACIFIC; PATTERNS; RIVER; PERIODICITY; RAINFALL}},
Research-Areas = {{Biodiversity \& Conservation; Environmental Sciences \& Ecology}},
Web-of-Science-Categories  = {{Biodiversity Conservation; Ecology; Environmental Sciences}},
Author-Email = {{mworbes@gwdg.de}},
ResearcherID-Numbers = {{Junk, Wolfgang J/A-6172-2017
   Piedade, Maria Teresa F/C-5372-2013
   Schongart, Jochen/I-2659-2016
   }},
ORCID-Numbers = {{Piedade, Maria Teresa F/0000-0002-7320-0498
   Schongart, Jochen/0000-0002-7696-9657}},
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Number-of-Cited-References = {{58}},
Times-Cited = {{111}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{41}},
Journal-ISO = {{Glob. Change Biol.}},
Doc-Delivery-Number = {{820WY}},
Unique-ID = {{ISI:000221421600011}},
DA = {{2020-08-06}},
}

@article{ ISI:000221524900011,
Author = {Graham, NE},
Title = {{Late-Holocene teleconnections between tropical Pacific climatic
   variability and precipitation in the western USA: evidence from proxy
   records}},
Journal = {{HOLOCENE}},
Year = {{2004}},
Volume = {{14}},
Number = {{3}},
Pages = {{436-447}},
Month = {{MAY}},
Abstract = {{Decadal to multidecadal fluctuations between drought and relatively more
   moist conditions are a defining characteristic of precipitation
   variability in the western USA. In an attempt to better understand the
   forcing mechanisms responsible for producing this variability,
   relationships between proxy indices of tropical climatic variability and
   precipitation-related reconstructions in the western USA are examined.
   The tropical proxies include the delta(18)O record from the Quelccaya
   ice cap (southern Subtropical Andes) and the lacustrine sedimentation
   record from Laguna Pallcacocha (near-equatorial Andes). The
   precipitation-related records are tree-ring reconstructions of river
   flow, drought severity and precipitation over the contiguo USA. One new
   finding is a consistent relation between decadal variability in El Nino
   activity and precipitation-related proxies through much of the western
   USA during the past 1200 years. Surprisingly, the proxy records do not
   show a systematic link between inferred El Nino activity and
   precipitation in the interior Southwest USA. A second new result is the
   existence of relationships at decadal- to multidecadal timescales
   between fluctuations in Quelccaya delta(18)O, precipitation-related
   proxies from the western USA, and proxy records from the Pacific Basin.
   This finding links the Quelccaya record to the transhemispheric Pacific
   decadal-scale climatic variability documented from proxy records by
   Villalba et al (2001), and suggests that similar changes in the
   large-scale circulation changes accompany both the decadal and
   multidecadal signals. A composite constructed using gridded proxy
   precipitation constructed on the basis of decadal-scale fluctuations in
   inferred-El Nino activity shows a pattern rather different to Nino-based
   teleconnection maps for the instrumental record. In the proxy-based
   composite, positive values cover much of the extreme western, west
   central and southeastern USA, with negative values in the central
   Mississippi Valley. The interior Southwest shows essentially no
   response. A second composite based on multidecadal variability in
   Quelccaya delta(18)O shows a well-developed dipole pattern across the
   western USA with opposing centres in the interior Southwest and
   Northwest. It is suggested that this dipole pattern results from
   multidecadal variability in tropical Pacific SSTs and resulting changes
   in the strength of the Northeast Pacific High and the latitudinal
   distribution of cool season westerlies across the eastern North Pacific
   and western USA.}},
Publisher = {{SAGE PUBLICATIONS LTD}},
Address = {{1 OLIVERS YARD, 55 CITY ROAD, LONDON EC1Y 1SP, ENGLAND}},
Type = {{Review}},
Language = {{English}},
Affiliation = {{Graham, NE (Corresponding Author), Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA.
   Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA.
   Hydrol Res Ctr, San Diego, CA 92130 USA.}},
DOI = {{10.1191/0959683604hl719xx}},
ISSN = {{0959-6836}},
EISSN = {{1477-0911}},
Keywords = {{tropical-mid-latitude teleconnections; El Nino; western USA
   precipitation; Andean ice cores; Andean lake cores; Holocene}},
Keywords-Plus = {{SEA-SURFACE TEMPERATURE; QUELCCAYA ICE CAP; EL-NINO; MODELING
   DELTA-O-18; ENSO; CALIFORNIA; CORES; RECONSTRUCTION; RAINFALL; AMERICA}},
Research-Areas = {{Physical Geography; Geology}},
Web-of-Science-Categories  = {{Geography, Physical; Geosciences, Multidisciplinary}},
Author-Email = {{ngraham@hrc-lab.org}},
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