text:
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Number-of-Cited-References = {{14}},
Times-Cited = {{123}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{37}},
Journal-ISO = {{Ecol. Econ.}},
Doc-Delivery-Number = {{620UM}},
Unique-ID = {{ISI:000179550900006}},
DA = {{2020-08-06}},
}

@article{ ISI:000179520200005,
Author = {Hoekstra, R and van den Bergh, JCJM},
Title = {{Structural decomposition analysis of physical flows in the economy}},
Journal = {{ENVIRONMENTAL \& RESOURCE ECONOMICS}},
Year = {{2002}},
Volume = {{23}},
Number = {{3}},
Pages = {{357-378}},
Month = {{NOV}},
Abstract = {{Many environmental problems can be attributed to the extraction and
   emissions of physical substances. Increasing our understanding of the
   economic and technological driving forces behind these physical flows
   can contribute to solving the environmental problems related to them.
   The input-output framework is a useful setting in which to integrate
   detailed information about economic structure and physical flows. In
   this article a specific method in input-output analysis is reviewed,
   namely Structural Decomposition Analysis (SDA). It is based on
   comparative static analysis, which decomposes historical changes of a
   policy variable into determinant effects. SDA has been applied, for
   example, to analyze the demand and technological driving forces of
   energy use, CO2-emissions and various other pollutants and resources.
   This article examines the theoretical aspects of structural
   decomposition, in particular those concerning physical flows and
   environmental issues. Furthermore, the article includes an extensive
   survey of empirical studies.}},
Publisher = {{SPRINGER}},
Address = {{VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Hoekstra, R (Corresponding Author), Free Univ Amsterdam, Dept Spatial Econ, De Boelelaan 1105, NL-1081 HV Amsterdam, Netherlands.
   Free Univ Amsterdam, Dept Spatial Econ, NL-1081 HV Amsterdam, Netherlands.}},
DOI = {{10.1023/A:1021234216845}},
ISSN = {{0924-6460}},
EISSN = {{1573-1502}},
Keywords = {{CO2-emissions; comparative static analysis; energy use; environmental
   analysis; input-output analysis; material flows; physical flows;
   structural change; technological change}},
Keywords-Plus = {{INDUSTRIAL ENERGY-CONSUMPTION; INTERCOUNTRY; EMISSION; TAIWAN}},
Research-Areas = {{Business \& Economics; Environmental Sciences \& Ecology}},
Web-of-Science-Categories  = {{Economics; Environmental Studies}},
Author-Email = {{rhoekstra@feweb.vu.nl
   jbergh@feweb.vu.nl}},
ResearcherID-Numbers = {{van den Bergh, Jeroen/C-7103-2008}},
ORCID-Numbers = {{Hoekstra, Rutger/0000-0001-6531-9782
   van den Bergh, Jeroen/0000-0003-3415-3083}},
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Number-of-Cited-References = {{69}},
Times-Cited = {{149}},
Usage-Count-Last-180-days = {{5}},
Usage-Count-Since-2013 = {{70}},
Journal-ISO = {{Environ. Resour. Econ.}},
Doc-Delivery-Number = {{620ED}},
Unique-ID = {{ISI:000179520200005}},
DA = {{2020-08-06}},
}

@article{ ISI:000180633400005,
Author = {Panagiotopoulos, F and Shahgedanova, M and Stephenson, DB},
Title = {{A review of Northern Hemisphere winter-time teleconnection patterns}},
Journal = {{JOURNAL DE PHYSIQUE IV}},
Year = {{2002}},
Volume = {{12}},
Number = {{PR10}},
Pages = {{27-47}},
Month = {{NOV}},
Note = {{European Research Course on Atmospheres, GRENOBLE, FRANCE, 2002}},
Abstract = {{This chapter reviews the major teleconnection patterns that occur in the
   boreal winter season. The history of teleconnection research is first
   reviewed emphasising the pioneering work of Sir Gilbert Walker. This is
   followed by a review of contemporary research that focuses on eleven
   teleconnection patterns classified into two groups: Euro-Atlantic and
   Pacific/North American patterns. Structure, impacts on weather and
   climate and temporal variability of each pattern are discussed by
   critically comparing major teleconnection studies. The lack of agreement
   on structure and occasionally the very existence of certain
   teleconnection patterns is also highlighted. These disagreements can be
   attributed to the absence of a universally accepted definition of
   teleconnections and the use of different statistical methods and data
   sets.}},
Publisher = {{EDP SCIENCES S A}},
Address = {{17, AVE DU HOGGAR, PA COURTABOEUF, BP 112, F-91944 LES ULIS CEDEX A,
   FRANCE}},
Type = {{Article; Proceedings Paper}},
Language = {{English}},
Affiliation = {{Panagiotopoulos, F (Corresponding Author), Univ Reading, Dept Geog, POB 227, Reading RG6 6AB, Berks, England.
   Univ Reading, Dept Geog, Reading RG6 6AB, Berks, England.
   Univ Reading, Dept Meteorol, Reading RG6 6BB, Berks, England.}},
DOI = {{10.1051/jp4:20020450}},
ISSN = {{1155-4339}},
Keywords-Plus = {{GEOPOTENTIAL HEIGHT FIELD; ATLANTIC OSCILLATION; EXTRATROPICAL
   CIRCULATION; SOUTHERN OSCILLATION; ENSEMBLE EXPERIMENTS; ARCTIC
   OSCILLATION; ANNULAR MODES; VARIABILITY; FREQUENCY; TEMPERATURES}},
Research-Areas = {{Physics}},
Web-of-Science-Categories  = {{Physics, Multidisciplinary}},
ResearcherID-Numbers = {{Stephenson, David/A-9903-2011}},
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Number-of-Cited-References = {{34}},
Times-Cited = {{31}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{13}},
Journal-ISO = {{J. Phys. IV}},
Doc-Delivery-Number = {{639MQ}},
Unique-ID = {{ISI:000180633400005}},
DA = {{2020-08-06}},
}

@article{ ISI:000178884800009,
Author = {Wang, B and Zhang, Q},
Title = {{Pacific-east Asian teleconnection. Part II: How the Philippine Sea
   anomalous anticyclone is established during El Nino development}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2002}},
Volume = {{15}},
Number = {{22}},
Pages = {{3252-3265}},
Month = {{NOV}},
Abstract = {{The anomalous Philippine Sea anticyclone (PSAC) conveys impacts of El
   Nino to east Asian climate during the mature and decay of an El Nino
   (from the winter to ensuing summer). It is shown that the anomalous PSAC
   forms in fall about one season prior to the peak El Nino; its strength
   increases with the El Nino intensity and its sign reverses during a La
   Nina. The PSAC formation concurs with abnormal deepening of the east
   Asian trough and with increasing number of northward recurvature of
   tropical storms in the western Pacific. The PSAC establishment is
   abrupt, coupling with a swing from a wet to dry phase of an
   intraseasonal oscillation (ISO) and often concurrent with early retreat
   of the east Asian summer monsoon. The ISO becomes inactive after PSAC
   establishment.
   The development of the PSAC is attributed to combined effects of the
   remote El Nino forcing, tropical-extratropical interaction, and
   monsoon-ocean interaction. The developing El Nino induces off-equatorial
   ascending Rossby wave responses and land surface cooling in northeast
   Asia; both deepen the east Asian trough in fall and induces vigorous
   tropical-extratropical exchange of air mass and heat, which enhances the
   cold air outbreak and initiation of the PSAC. Through exciting
   descending Rossby waves, the El Nino-induced Indonesian subsidence
   generates low-level anticyclonic vorticity over south Asia, which is
   advected by mean monsoon westerly, instigating the anomalous PSAC. The
   ISO interacting with the underlying ocean plays a critical role in the
   abrupt establishment of PSAC. The wind-evaporation/entrainment feedback
   tends to amplify (suppress) ISO before (after) winter northeasterly
   monsoon commences, suggesting the roles of atmosphere-ocean interaction
   and the seasonal march of background winds in changing the Philippine
   Sea ISO intensity and maintaining PSAC.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Wang, B (Corresponding Author), Univ Hawaii Manoa, Sch Ocean \& Earth Sci \& Technol, Dept Meteorol, 2525 Correa Rd, Honolulu, HI 96822 USA.
   Univ Hawaii Manoa, Sch Ocean \& Earth Sci \& Technol, Dept Meteorol, Honolulu, HI 96822 USA.}},
DOI = {{10.1175/1520-0442(2002)015<3252:PEATPI>2.0.CO;2}},
ISSN = {{0894-8755}},
Keywords-Plus = {{WESTERN NORTH PACIFIC; SUMMER INTRASEASONAL OSCILLATION; INTERDECADAL
   VARIATIONS; TROPICAL PACIFIC; EQUATORIAL WAVES; MONSOON; ENSO;
   VARIABILITY; IMPACT; CIRCULATION}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
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Number-of-Cited-References = {{40}},
Times-Cited = {{282}},
Usage-Count-Last-180-days = {{3}},
Usage-Count-Since-2013 = {{63}},
Journal-ISO = {{J. Clim.}},
Doc-Delivery-Number = {{609CJ}},
Unique-ID = {{ISI:000178884800009}},
DA = {{2020-08-06}},
}

@article{ ISI:000177828000003,
Author = {Bratti, M},
Title = {{Does the choice of university matter? A study of the differences across
   UK universities in life sciences students' degree performance}},
Journal = {{ECONOMICS OF EDUCATION REVIEW}},
Year = {{2002}},
Volume = {{21}},
Number = {{5}},
Pages = {{431-443}},
Month = {{OCT}},
Abstract = {{This paper investigates differences across UK universities in 1993 life
   sciences students' degree performance using individual-level data from
   the Universities' Statistical Record (USR). Differences across
   universities are analysed by specifying and estimating a
   subject-specific educational production function. Even after including a
   wide range of controls for the quality of students, significant
   differences emerge across universities in students' degree performance.
   We apply a two-stage estimation procedure and find evidence that a large
   part Of `university effects' cannot be explained by the kind of
   institutional inputs commonly used in the literature on school quality.
   Finally, we compare the unadjusted ranking of universities based on the
   proportion of `good' (first and upper second class honours) degrees
   awarded with that based on the estimated probability of a `good' degree
   obtained from the microeconometric model and find significant
   differences between the two indicators of universities' performance. (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 = {{Bratti, M (Corresponding Author), Univ Warwick, Coventry CV4 7AL, W Midlands, England.
   Univ Warwick, Coventry CV4 7AL, W Midlands, England.
   Univ Ancona, I-60121 Ancona, Italy.}},
DOI = {{10.1016/S0272-7757(01)00035-8}},
Article-Number = {{PII S0272-7757(01)00035-8}},
ISSN = {{0272-7757}},
Keywords = {{educational economics; input-output analysis; ordered probit;
   performance indicators; value-added}},
Keywords-Plus = {{EDUCATION; DEMAND}},
Research-Areas = {{Business \& Economics; Education \& Educational Research}},
Web-of-Science-Categories  = {{Economics; Education \& Educational Research}},
ResearcherID-Numbers = {{Bratti, Massimiliano/J-6811-2012}},
ORCID-Numbers = {{Bratti, Massimiliano/0000-0002-4565-6260}},
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Number-of-Cited-References = {{38}},
Times-Cited = {{21}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{12}},
Journal-ISO = {{Econ. Educ. Rev.}},
Doc-Delivery-Number = {{590NB}},
Unique-ID = {{ISI:000177828000003}},
DA = {{2020-08-06}},
}

@article{ ISI:000179273400009,
Author = {Bradbury, JA and Dingman, SL and Keim, BD},
Title = {{New England drought and relations with large scale atmospheric
   circulation patterns}},
Journal = {{JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION}},
Year = {{2002}},
Volume = {{38}},
Number = {{5}},
Pages = {{1287-1299}},
Month = {{OCT}},
Abstract = {{To provide a basis for regional hydroclimatic forecasting, New England
   (NE) precipitation and streamflow are compared with indices for the El
   Nino/Southern Oscillation, the Pacific North American (PNA) pattern, and
   the North Atlantic Oscillation (NAO). Significant positive correlations
   are found between the NAO index and monthly streamflow at western inland
   locations, with the strongest seasonal correlations occurring in winter.
   Smoothed records for the winter NAO and winter streamflow are highly
   correlated at some sites, suggesting that interrelationships are most
   significant in the low frequency spectrum. However, correlations between
   the NAO and precipitation are not significant, so further examination of
   other factors is needed to explain the relationship between the NAO and
   streamflow. NAO related regional air temperature, sea surface
   temperature (SST), storm tracking, and snowfall variability are possible
   mechanisms for the observed teleconnection. Exceptionally cool regional
   air temperatures, and SSTs, and unique regional storm track patterns
   characterized NE's climate during the famous 1960s drought, suggesting
   that concurrent (persistent) negative NAO conditions may have
   contributed to the severity of that event. Monthly and winter averaged
   regional streamflow variability are also significantly correlated with
   the PNA index. This, along with results from previous studies, suggests
   that tropospheric wave character and associated North Pacific SST
   anomalies are also related to NE regional drought conditions.}},
Publisher = {{AMER WATER RESOURCES ASSOC}},
Address = {{4 WEST FEDERAL ST, PO BOX 1626, MIDDLEBURG, VA 20118-1626 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Bradbury, JA (Corresponding Author), Univ New Hampshire, Inst Study Earth Oceans \& Space, Climate Change Res Ctr, Durham, NH 03824 USA.
   Univ New Hampshire, Inst Study Earth Oceans \& Space, Climate Change Res Ctr, Durham, NH 03824 USA.
   Univ New Hampshire, Dept Earth Sci, Durham, NH 03824 USA.}},
DOI = {{10.1111/j.1752-1688.2002.tb04348.x}},
ISSN = {{1093-474X}},
Keywords = {{hydroclimate; New England; drought; North Atlantic Oscillation; Pacific
   North American pattern}},
Keywords-Plus = {{NORTH-ATLANTIC OSCILLATION; AMERICAN TELECONNECTION PATTERN; NINO
   SOUTHERN OSCILLATION; UNITED-STATES STREAMFLOW; CLIMATE; VARIABILITY;
   HEMISPHERE; WINTER; PRECIPITATION; PACIFIC}},
Research-Areas = {{Engineering; Geology; Water Resources}},
Web-of-Science-Categories  = {{Engineering, Environmental; Geosciences, Multidisciplinary; Water
   Resources}},
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Number-of-Cited-References = {{45}},
Times-Cited = {{61}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{16}},
Journal-ISO = {{J. Am. Water Resour. Assoc.}},
Doc-Delivery-Number = {{615XV}},
Unique-ID = {{ISI:000179273400009}},
DA = {{2020-08-06}},
}

@article{ ISI:000178006500001,
Author = {Frederiksen, JS},
Title = {{Genesis of intraseasonal oscillations and equatorial waves}},
Journal = {{JOURNAL OF THE ATMOSPHERIC SCIENCES}},
Year = {{2002}},
Volume = {{59}},
Number = {{19}},
Pages = {{2761-2781}},
Month = {{OCT}},
Abstract = {{The particular role of evaporation-wind feedback, and as well cumulus
   convection and dissipation, in the formation of the Madden-Julian
   30-60-day intraseasonal oscillation (MJO) and equatorially trapped
   waves, including Kelvin, equatorial Rossby, mixed Rossby-gravity, and
   eastward inertio-gravity waves, has been studied using a global
   two-level primitive equation instability model. The evaporation has been
   specified through a bulk aerodynamic formula, and the convection through
   a generalized Kuo-type parameterization with a moist static stability
   that is positive everywhere so that wave-conditional instability of the
   second kind (CISK) is not possible. Both three-dimensional and zonally
   averaged basic states for January 1979 have been employed, and the
   e-folding times, periods, structures, and propagation characteristics of
   these waves have been analyzed and compared with their observed
   properties.
   The MJO modes appear to be particularly realistic when the
   three-dimensional basic state includes evaporation-wind feedback, which
   promotes the zonal wavenumber-1 component of the eastward-propagating
   velocity potential, and cumulus convection. The tropical velocity
   potential propagates eastward relatively quickly around the globe
   (approximate to13.6 m s(-1), corresponding to a period of 34.4 days),
   while in the convective region between the Indian Ocean and the date
   line the divergence propagates more slowly (approximate to4.5 m s(-1)).
   The MJO has a largely first internal mode structure in the Tropics with
   a more equivalent barotropic structure of the streamfunction in the
   extratropics, including distinct Pacific-North American and Eurasian
   patterns. The MJO modes do not lie along any of the theoretical
   dispersion curves of equatorially trapped waves and have distinctly
   longer periods than the model convectively coupled Kelvin waves, even at
   zonal wavenumber 1, as in the observational study of M. Wheeler and G.
   N. Kiladis. The Kelvin mode streamfunction fields also do not exhibit
   the largely equivalent barotropic teleconnection patterns in the
   extratropics typical of the MJO. With cumulus convection and
   evaporation-wind feedback, the model equatorially trapped Kelvin,
   equatorial Rossby, mixed Rossby-gravity, and eastward inertio-gravity
   waves have periods, structures, and propagation characteristics
   comparable to those of corresponding convectively coupled observed
   waves.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Frederiksen, JS (Corresponding Author), CSIRO, Private Mail Bag 1, Aspendale, Vic 3195, Australia.
   CSIRO, Aspendale, Vic 3195, Australia.}},
DOI = {{10.1175/1520-0469(2002)059<2761:GOIOAE>2.0.CO;2}},
ISSN = {{0022-4928}},
Keywords-Plus = {{TROPICAL-EXTRATROPICAL INTERACTION; GENERAL-CIRCULATION MODEL;
   EVAPORATION-WIND FEEDBACK; MADDEN-JULIAN OSCILLATION; 40-50 DAY
   OSCILLATION; AIR-SEA INTERACTION; SHEARED ZONAL FLOW; LOW-FREQUENCY;
   TELECONNECTION PATTERNS; CONVECTIVE ADJUSTMENT}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
ORCID-Numbers = {{Frederiksen, Jorgen/0000-0001-9449-0968}},
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Number-of-Cited-References = {{72}},
Times-Cited = {{22}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{5}},
Journal-ISO = {{J. Atmos. Sci.}},
Doc-Delivery-Number = {{593RR}},
Unique-ID = {{ISI:000178006500001}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000178031400002,
Author = {Franzke, C},
Title = {{Dynamics of low-frequency variability: Barotropic mode}},
Journal = {{JOURNAL OF THE ATMOSPHERIC SCIENCES}},
Year = {{2002}},
Volume = {{59}},
Number = {{20}},
Pages = {{2897-2909}},
Month = {{OCT}},
Abstract = {{The dynamics of low-frequency variability is investigated in terms of
   sensitivity to the dependence of its relative zonal position of a single
   storm track in a simplified global circulation model. A streamfunction
   tendency equation is derived that explicitly distinguishes between
   barotropic and baroclinic components. One of the two low-frequency
   patterns located in the center of the storm track grows barotropically,
   and its decay is accomplished by low-frequency eddy vorticity fluxes and
   the baroclinic contribution to the divergence term. The growth and decay
   of the second pattern, located at the downstream end of the storm track,
   is dominated by nonlinear processes. This indicates that the dynamical
   processes leading to growth and decay of low-frequency patterns depend
   on the zonal position of the low-frequency pattern relative to a storm
   track.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Franzke, C (Corresponding Author), Penn State Univ, EMS Environm Inst, 2217 Earth \& Engn Sci Bldg, University Pk, PA 16802 USA.
   Penn State Univ, EMS Environm Inst, University Pk, PA 16802 USA.}},
DOI = {{10.1175/1520-0469(2002)059<2897:DOLFVB>2.0.CO;2}},
ISSN = {{0022-4928}},
Keywords-Plus = {{GLOBAL CIRCULATION MODEL; NORTH PACIFIC-OCEAN; TELECONNECTION PATTERNS;
   STORM TRACKS; NONLINEAR MODEL; LIFE-CYCLES; ATMOSPHERE; ANOMALIES;
   HEMISPHERE; CYCLOGENESIS}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
ResearcherID-Numbers = {{Franzke, Christian L E/A-6191-2012}},
ORCID-Numbers = {{Franzke, Christian L E/0000-0003-4111-1228}},
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Number-of-Cited-References = {{35}},
Times-Cited = {{12}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{5}},
Journal-ISO = {{J. Atmos. Sci.}},
Doc-Delivery-Number = {{594CP}},
Unique-ID = {{ISI:000178031400002}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000179961200004,
Author = {Li, T and Zhang, YS},
Title = {{Processes that determine the quasi-biennial and lower-frequency
   variability of the South Asian monsoon}},
Journal = {{JOURNAL OF THE METEOROLOGICAL SOCIETY OF JAPAN}},
Year = {{2002}},
Volume = {{80}},
Number = {{5}},
Pages = {{1149-1163}},
Month = {{OCT}},
Abstract = {{The spatial and temporal structures of atmospheric circulation and SST
   associated with the Indian monsoon rainfall variability on
   quasi-biennial (2-3 year) and lower-frequency (3-7 year) time scales
   were investigated, using the domain-averaged Indian rainfall, the
   NCAR/NCEP reanalysis and Reynolds SST data. We took both time-filtering
   and composite analysis approaches. The results indicate that physical
   processes that determine the monsoon rainfall variation on the 2-3 year
   and 3-7 year time scales are different. The quasi-biennial variability
   of the monsoon is primarily determined by local processes in the Indian
   Ocean. Both local SST and moisture flux convergence anomalies are highly
   correlated with the monsoon at a lagged time of 3-6 months. It is argued
   that a positive SST anomaly in the Indian Ocean increases local moisture
   due to enhanced surface evaporation. The accumulation of these moistures
   leads to a strong monsoon through anomalous moisture advection by summer
   mean flows.
   The lower-frequency variability of the monsoon is primarily attributed
   to remote forcing mechanisms. Three possible processes may contribute to
   the monsoon variability on the 3-7 year time scale. The first is through
   the change of large-scale, east-west circulation induced by the eastern
   Pacific SST anomaly. The second is attributed to the effect of the SST
   anomaly in the Northwestern Pacific through enhanced (or suppressed)
   convective activity along the monsoon trough. The third is attributed to
   the tropical-midlatitude teleconnection-a strong north-south, land-ocean
   thermal contrast occurs six months prior to a wet monsoon, and it
   persists from the preceding winter to summer and is responsible for the
   monsoon intensity change.}},
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 = {{Li, T (Corresponding Author), Univ Hawaii, Dept Meteorol, 2525 Correa Rd, Honolulu, HI 96822 USA.
   Univ Hawaii, Dept Meteorol, Honolulu, HI 96822 USA.
   Univ Hawaii, Int Pacific Res Ctr, Honolulu, HI 96822 USA.}},
DOI = {{10.2151/jmsj.80.1149}},
ISSN = {{0026-1165}},
EISSN = {{2186-9057}},
Keywords-Plus = {{SEA-SURFACE TEMPERATURE; SUMMER MONSOON; INTERANNUAL VARIABILITY;
   TROPICAL PACIFIC; INDIAN MONSOON; WINTER MONSOON; ANNUAL CYCLE; OCEAN;
   ENSO; PREDICTABILITY}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{timli@hawaii.edu}},
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Number-of-Cited-References = {{40}},
Times-Cited = {{30}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{3}},
Journal-ISO = {{J. Meteorol. Soc. Jpn.}},
Doc-Delivery-Number = {{627XF}},
Unique-ID = {{ISI:000179961200004}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000179072700009,
Author = {Norris, GA},
Title = {{Life cycle emission distributions within the economy: Implications for
   life cycle impact assessment}},
Journal = {{RISK ANALYSIS}},
Year = {{2002}},
Volume = {{22}},
Number = {{5}},
Pages = {{919-930}},
Month = {{OCT}},
Abstract = {{Refinements of methods for life cycle impact assessment (LCIA) are
   directed at removing unjustified simplifications and quantifying and
   reducing uncertainties in results. The amount of uncertainty reduction
   that is actually achieved through LCIA method refinement depends on the
   structure of the life cycle inventory model. We investigate the general
   structure of inventory models using an economic input/output (I/O) life
   cycle assessment model of the US. economy. In particular, we study the
   results of applying a streamlining algorithm to the I/O LCA model. The
   streamlining algorithm retains only those ``branches{''} of the process
   tree that are jointly required to account for a specified fraction of
   the total impacts upstream of each point in the tree. We examine the
   implications of these ``tree pruning{''} results for site-informed LCIA.
   Percentiles are presented for U.S. commodities and several important
   pollutants, for the share of total upstream emissions contributed by the
   set of processes in each supply tier, that is, each set of processes
   that directly supply inputs to another set of processes. Capturing at
   least 90\% of the total direct plus upstream emissions for criteria air
   pollutants and toxic releases for at least 75\% of the commodities in
   the U.S. economy requires full modeling of direct emissions plus the
   first five supply tiers. The requirements for capturing a high
   percentage (e.g., >80\%) of total emissions vary widely across products
   or commodities. To capture more than 60\% of total emissions for more
   than half of all commodities requires models with more than 4,000
   process instances. To well characterize the total impacts of products,
   life cycle impact assessment methods must characterize foreground
   process impacts in a site-informed way and mean impacts of far-removed
   processes in an unbiased way.}},
Publisher = {{BLACKWELL PUBLISHERS}},
Address = {{350 MAIN STREET, STE 6, MALDEN, MA 02148 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Norris, GA (Corresponding Author), Sylvatica, 147 Bauneg Hill Rd, North Berwick, ME 03906 USA.
   Sylvatica, North Berwick, ME 03906 USA.
   Harvard Univ, Sch Publ Hlth, Boston, MA 02115 USA.}},
DOI = {{10.1111/1539-6924.00261}},
ISSN = {{0272-4332}},
Keywords = {{life cycle assessment; life cycle inventory analysis; uncertainty
   analysis; boundary truncation; input/output analysis; impact assessment;
   streamlining}},
Keywords-Plus = {{GENERIC SPATIAL CLASSES; HUMAN HEALTH IMPACTS}},
Research-Areas = {{Public, Environmental \& Occupational Health; Mathematics; Mathematical
   Methods In Social Sciences}},
Web-of-Science-Categories  = {{Public, Environmental \& Occupational Health; Mathematics,
   Interdisciplinary Applications; Social Sciences, Mathematical Methods}},
Cited-References = {{Curtiss PS, 1996, ATMOS ENVIRON, V30, P3331, DOI 10.1016/1352-2310(96)00031-3.
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   {*}US EPA, 2001, TOX REL INV HOM WEBS.}},
Number-of-Cited-References = {{21}},
Times-Cited = {{14}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{9}},
Journal-ISO = {{Risk Anal.}},
Doc-Delivery-Number = {{612KB}},
Unique-ID = {{ISI:000179072700009}},
DA = {{2020-08-06}},
}

@article{ ISI:000177901000005,
Author = {Su, H and Neelin, JD},
Title = {{Teleconnection mechanisms for tropical Pacific descent anomalies during
   El Nino}},
Journal = {{JOURNAL OF THE ATMOSPHERIC SCIENCES}},
Year = {{2002}},
Volume = {{59}},
Number = {{18}},
Pages = {{2694-2712}},
Month = {{SEP 15}},
Abstract = {{Teleconnection mechanisms in relative descent zones are examined using
   the quasi-equilibrium tropical circulation model (QTCM). The regions of
   anomalous descent neighboring the warm sea surface temperature (SST)
   anomalies in the eastern and central Pacific Ocean during the 1997/98 El
   Nino are used as an example, and results are verified for three other El
   Nino warm events (1982, 1987, and 1991). By analyzing the moisture and
   moist static energy budgets over these regions, it is found that the
   physical processes responsible for the descent anomalies are different
   for each region. Anomalous dry advection is the dominant mechanism for
   the reduced precipitation to the north of the El Nino warm region. On
   the other hand, the relative descent to the south of the El Nino warm
   SSTs is caused by reduced surface wind speed and reduced air-sea
   contrast and resulting weaker than normal evaporation. Budget analysis
   based on the National Aeronautics and Space Administration
   Seasonal-to-Interannual Prediction Project atmospheric general
   circulation model simulations is consistent with the QTCM results.
   Radiative cooling associated with the warming of tropospheric
   temperature is relatively small, on the order of a few watts per square
   meter. The traditional assumption that compensating subsidence is caused
   by radiative cooling due to increased tropospheric temperature thus does
   not apply in this context. An experiment to test this by suppressing the
   radiative cooling due to temperature anomalies showed little impact on
   the descent anomalies. Thus radiative cooling is not even an initiator
   of descent anomalies. Instead, relative descent tends to occur in
   particular regions where other larger cooling or drying tendencies act.
   Reductions in convective heating and cloud radiative heating behave like
   a reduction in effective static stability, enhancing the descent
   anomalies. The complexity of the mechanisms for the descent anomalies
   may be responsible for the difficulty of descent zone simulation and
   forecast in general circulation models.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Neelin, JD (Corresponding Author), Univ Calif Los Angeles, Dept Atmospher Sci, Inst Geophys \& Planetary Phys, Los Angeles, CA 90095 USA.
   Univ Calif Los Angeles, Dept Atmospher Sci, Inst Geophys \& Planetary Phys, Los Angeles, CA 90095 USA.}},
DOI = {{10.1175/1520-0469(2002)059<2694:TMFTPD>2.0.CO;2}},
ISSN = {{0022-4928}},
Keywords-Plus = {{SEA-SURFACE TEMPERATURES; CIRCULATION MODEL; SOUTHERN OSCILLATION;
   ATMOSPHERIC RESPONSE; RAINFALL ANOMALIES; HYDROLOGICAL CYCLE; SST
   ANOMALIES; INDIAN-OCEAN; ENSO; PRECIPITATION}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{neelin@atmos.ucla.edu}},
ResearcherID-Numbers = {{Neelin, J. David/H-4337-2011}},
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Number-of-Cited-References = {{46}},
Times-Cited = {{78}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{12}},
Journal-ISO = {{J. Atmos. Sci.}},
Doc-Delivery-Number = {{591VM}},
Unique-ID = {{ISI:000177901000005}},
DA = {{2020-08-06}},
}

@article{ ISI:000178145700004,
Author = {Rogers, JC and McHugh, MJ},
Title = {{On the separability of the North Atlantic oscillation and Arctic
   oscillation}},
Journal = {{CLIMATE DYNAMICS}},
Year = {{2002}},
Volume = {{19}},
Number = {{7}},
Pages = {{599-608}},
Month = {{SEP}},
Abstract = {{We address the issue of whether the Arctic (AO), and North Atlantic
   oscillations (NAO) are inseparable, forming an annular mode in the
   Northern Hemisphere atmospheric circulation. This annular mode is the
   leading empirical orthogonal function of hemispheric sea level pressure
   (SLP) data, explaining the largest amount of its variability. We examine
   whether the NAO and AO are inseparable spatial modes of the atmospheric
   circulation using rotated principal component analysis (RPCA), a
   methodology that identifies simple and unique patterns of spatial
   dataset variability. RPCA of the spring, summer, and autumn SLP fields
   from

path: /data/wos_io/savedrecs (13).bib

filename: savedrecs (13).bib