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Number-of-Cited-References = {{18}},
Times-Cited = {{3}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{3}},
Journal-ISO = {{Adv. Atmos. Sci.}},
Doc-Delivery-Number = {{577RQ}},
Unique-ID = {{ISI:000177075900002}},
DA = {{2020-08-06}},
}

@article{ ISI:000178155100004,
Author = {Huang, F and Zhou, FX and Qian, XD},
Title = {{Interannual and decadal variability of the North Pacific blocking and
   its relationship to SST, teleconnection and storm tracks}},
Journal = {{ADVANCES IN ATMOSPHERIC SCIENCES}},
Year = {{2002}},
Volume = {{19}},
Number = {{5}},
Pages = {{807-819}},
Abstract = {{Climatological features of mid-latitude blocking occurring over the
   North Pacific Ocean during 52 winters (December to February) of 1948 /
   1949-1999/ 2000 are statistically analyzed based on NCEP/ NCAR
   reanalysis data. Significant interannual variation with a period of
   about 3-7 years as well as decadal variability is found by wavelet
   analysis and power spectrum analysis. A decreasing trend of the 2-7 year
   bandscale-averaged variance occurs throughout the 52 years and an abrupt
   shift from a higher state to a lower state during the 1970s is also
   found, which suggests an interdecadal variation of the North Pacific
   blocking, The possible relationship between the variability of blocking
   and sea Surface temperature (SST), storm tracks and teleconnection are
   shown using composite analysis. In strong blocking anomaly winter (SBW),
   the geopotential height anomaly at 500 hPa exhibits a typical PNA
   (Pacific-North American)-like wave-train pattern in the North Pacific,
   The storm tracks, representing the activity of transient eddies, extend
   northeastward to the western coast of North America along the mid
   latitudes of about 40degrees-50degreesN, with the SST anomaly exhibiting
   a Pacific decadal oscillation (PDO) mode at mid-latitude and a La
   Nina-like pattern along the equator. Contrasting features appear in weak
   blocking anomaly winter (WBW).}},
Publisher = {{SCIENCE PRESS}},
Address = {{16 DONGHUANGCHENGGEN NORTH ST, BEIJING 100717, PEOPLES R CHINA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Huang, F (Corresponding Author), Ocean Univ Qingdao, Dept Marine Meteorol, Qingdao 266003, Peoples R China.
   Ocean Univ Qingdao, Dept Marine Meteorol, Qingdao 266003, Peoples R China.}},
ISSN = {{0256-1530}},
EISSN = {{1861-9533}},
Keywords = {{north Pacific blocking; teleconnection; SST anomaly; and storm tracks}},
Keywords-Plus = {{SEA-SURFACE TEMPERATURE; ATMOSPHERIC GENERAL-CIRCULATION; DATA
   ASSIMILATION ANALYSIS; UPPER OCEAN 1950-95; PLANETARY-SCALE; EL-NINO;
   SOUTHERN OSCILLATION; TRANSIENT EDDIES; HIGH-FREQUENCY; ANOMALIES}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{huangf@mail.ouqd.edu.cn}},
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Number-of-Cited-References = {{45}},
Times-Cited = {{9}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{8}},
Journal-ISO = {{Adv. Atmos. Sci.}},
Doc-Delivery-Number = {{596GB}},
Unique-ID = {{ISI:000178155100004}},
DA = {{2020-08-06}},
}

@inproceedings{ ISI:000182023600045,
Author = {Wang, NL and Yao, TD and Thompson, LG and Davis, ME},
Editor = {{Wolff, EW}},
Title = {{Indian monsoon and North Atlantic Oscillation signals reflected by Cl-
   and Na+ in a shallow ice core from Dasuopu Glacier, Xixabangma, Himalaya}},
Booktitle = {{ANNALS OF GLACIOLOGY, VOL 35}},
Series = {{Annals of Glaciology-Series}},
Year = {{2002}},
Volume = {{35}},
Pages = {{273-277}},
Note = {{International Symposium on Ice Cores and Climate, KANGERLUSSUAQ,
   GREENLAND, AUG 19-23, 2001}},
Abstract = {{Information about past atmospheric circulation and climate change can be
   revealed by the chemical constituents of ice cores. Based on the
   analytical results of Cl- and Na+ concentrations in an 18.5 m ice core,
   which contains 14 annual layers, from the Dasuopu glacier, central
   Himalaya, a significant correlation is found between Cl- and Na+
   concentrations. This, along with the average Cl-/Na+ weight ratio of
   1.9, indicates that moisture at the drilling site came mostly from
   oceans. Furthermore, there was a high positive correlation between the
   Cl-/Na+ ratio in the summer monsoon layers and the monsoon rainfall in
   northeast India, and there exists a teleconnection between the Cl- and
   Na+ concentrations in this shallow ice core and the North Atlantic
   Oscillation.}},
Publisher = {{INT GLACIOLOGICAL SOC}},
Address = {{LENSFIELD RD, CAMBRIDGE CB2 1ER, ENGLAND}},
Type = {{Article; Proceedings Paper}},
Language = {{English}},
Affiliation = {{Wang, NL (Corresponding Author), Chinese Acad Sci, Cold \& Arid Regions Environm \& Engn Res Inst, Lab Ice Core \& Cold Regions Environm, Lanzhou 730000, Peoples R China.
   Chinese Acad Sci, Cold \& Arid Regions Environm \& Engn Res Inst, Lab Ice Core \& Cold Regions Environm, Lanzhou 730000, Peoples R China.
   Ohio State Univ, Byrd Polar Res Ctr, Columbus, OH 43210 USA.}},
ISSN = {{0260-3055}},
ISBN = {{0-946417-30-X}},
Keywords-Plus = {{ATMOSPHERIC CIRCULATION; CHEMICAL-COMPOSITION; RECORD; AEROSOL; SNOW;
   CHEMISTRY; VOLCANISM; CLIMATE; SULFATE; SUMMIT}},
Research-Areas = {{Geology}},
Web-of-Science-Categories  = {{Geosciences, Multidisciplinary}},
Author-Email = {{nlwang@ns.lzb.ac.cn}},
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Number-of-Cited-References = {{38}},
Times-Cited = {{10}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{4}},
Doc-Delivery-Number = {{BW44W}},
Unique-ID = {{ISI:000182023600045}},
DA = {{2020-08-06}},
}

@article{ ISI:000174236200005,
Author = {Compagnucci, RH and Agosta, EA and Vargas, WM},
Title = {{Climatic change and quasi-oscillations in central-west Argentina summer
   precipitation: main features and coherent behaviour with southern
   African region}},
Journal = {{CLIMATE DYNAMICS}},
Year = {{2002}},
Volume = {{18}},
Number = {{5}},
Pages = {{421-435}},
Month = {{JAN}},
Abstract = {{Summer rainfall variability (October to March) shows inter-annual to
   multi-decadal fluctuations over a vast area of subtropical Argentina
   between 28degreesS-38degreesS and 65degreesW-70degreesW. Statistically
   significant oscillations of quasi-period in the bands of 18-21, 6, 4 and
   2 years can be found throughout the region and intra-regionally, though
   the latter are variable. The lower frequency variation produces
   alternating episodes of above and below normal rainfall each lasting
   roughly 9 years. This quasi-fluctuation appears to be shared with the
   summer rainfall region of South Africa and were in-phase related one
   another until mid-1970s. The teleconnection between both subtropical
   regions could be generated by an atmospheric-oceanic bridge through the
   global sea surface temperatures (SSTs), particularly those of the
   equatorial-tropical South Atlantic. From mid-1970s, the alternating wet
   and dry pattern has been interrupted in the Argentine region producing
   the longest, as yet unfinished, wet spell of the century, Thus, a
   significant change of the long-term variation was observed around 1977
   toward lower frequencies. Since then the statistical model that explains
   more than 89\% of the variance of the series until 1977, diverges from
   the observed values in the 1980s and 1990s. In addition the Yamamoto
   statistical index, employed to detect a climatic jump, reaches its major
   value in 1973 at the beginning of the current long wet spell. Therefore
   the change could be located between 1973 and 1977. Application of the
   t-student's test gives significant differences of mean values or
   pre-1977 and post-1977 sub-samples from both individual time series and
   the regional index series. The spectral analysis also shows changes in
   energy bands in concordance with the features of the change that
   occurred from mid-1970s. The change gives rise to a significant
   increment of more than 20\% in average of normal rainfall over the
   region. Conversely, a drought between mid-1980s and the 1990s has been
   observed in the South African counterpart with severe characteristics,
   thereby continuing the quasi-18-year oscillation. Consequently, the
   low-frequency coherent behaviour between both the Argentine and South
   African regions is lost from the mid-1970s. The analysis of association
   of wet/dry spells and warm/cold, El Nino/La Nina episodes appears to be
   not significant at scales of year-to-year variability although at
   decadal to multi-decadal scales the association could be relevant. More
   than one process of multi-decadal variability of global SSTs could
   influence the Argentine summer rainfall region and the former bi-decadal
   teleconnection. Finally, potential hypothetical factors of change are
   discussed, such as the strengthening of direct and indirect mechanisms
   of moisture flux transport associated with global warming, low-level
   atmospheric circulation changes and/or to SSTs mean condition long-term
   variations over tropical and subtropical South Atlantic and South
   Pacific oceans.}},
Publisher = {{SPRINGER-VERLAG}},
Address = {{175 FIFTH AVE, NEW YORK, NY 10010 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Compagnucci, RH (Corresponding Author), Univ Buenos Aires, Fac Ciencias Exactas \& Nat, Dept Ciencias Atmosfera \& Oceanos, RA-1428 Buenos Aires, DF, Argentina.
   Univ Buenos Aires, Fac Ciencias Exactas \& Nat, Dept Ciencias Atmosfera \& Oceanos, RA-1428 Buenos Aires, DF, Argentina.
   Consejo Nacl Invest Cient \& Tecn, RA-1033 Buenos Aires, DF, Argentina.}},
DOI = {{10.1007/s003820100183}},
ISSN = {{0930-7575}},
Keywords-Plus = {{SEA-SURFACE TEMPERATURE; EL-NINO; ANNUAL CYCLE; RAINFALL; VARIABILITY;
   ANOMALIES; HEMISPHERE; DROUGHTS; PACIFIC; IMPACT}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
ORCID-Numbers = {{Agosta, Eduardo/0000-0003-1182-8877}},
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Number-of-Cited-References = {{49}},
Times-Cited = {{50}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{2}},
Journal-ISO = {{Clim. Dyn.}},
Doc-Delivery-Number = {{528GN}},
Unique-ID = {{ISI:000174236200005}},
DA = {{2020-08-06}},
}

@article{ ISI:000179008300023,
Author = {Wong, CS and Crawford, DW},
Title = {{Flux of particulate inorganic carbon to the deep subarctic Pacific
   correlates with El Nino}},
Journal = {{DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY}},
Year = {{2002}},
Volume = {{49}},
Number = {{24-25}},
Pages = {{5705-5715}},
Abstract = {{Time-series data are presented from sequentially operating deep (3800m)
   sediment traps deployed continuously in the northeastern subarctic
   Pacific between 1982 and 1990. These data show that monthly anomalies in
   the fluxes of particulate organic carbon (POC) and particulate inorganic
   carbon (PIC) were significantly correlated with equatorial surface-water
   temperature anomaly (Ni (n) over tildeo 3.4 index). This
   ``teleconnection{''} was stronger for PIC than for POC, and average PIC
   flux almost doubled from 3.60 to 6.41 mg C m(-2) d(-1) during the years
   influenced by El Ni (n) over tildeo. Average POC flux increased from
   2.28 to 3.18 mg C m(-1) d(-1) during these same years influenced by El
   Ni (n) over tildeo, although interpretation of this average was
   complicated by a single high-flux event in August 1983. Rain ratio (mean
   daily PIC:POC flux) was approximate to25\% higher (increased from 1.70
   to 2.17) during the years influenced by El Ni (n) over tildeo. Oceanic
   sequestration of atmospheric CO2 is particularly sensitive to the rain
   ratio in the long term, and a decrease in PIC deposition of only 40\%
   has been invoked as sufficient to decrease atmospheric CO2 to the
   glacial value. An improved mechanistic understanding of the primary
   formation and sinking of PIC should help to unravel some of the poorly
   understood biogeochemical feedbacks operating on ocean/atmosphere
   exchange of CO2 over contemporary and geological time scales. (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 = {{Wong, CS (Corresponding Author), Fisheries Oceans Canada Inst Ocean Sci, Ctr Ocean Climate Chem, POB 6000, Sidney, BC V8L 4B2, Canada.
   Fisheries Oceans Canada Inst Ocean Sci, Ctr Ocean Climate Chem, Sidney, BC V8L 4B2, Canada.}},
DOI = {{10.1016/S0967-0645(02)00210-2}},
Article-Number = {{PII S0967-0645(02)00210-2}},
ISSN = {{0967-0645}},
EISSN = {{1879-0100}},
Keywords-Plus = {{EMILIANIA-HUXLEYI; CALCITE LYSOCLINE; NORTH-ATLANTIC; OCEAN; IRON;
   VARIABILITY; BLOOMS; COCCOLITHOPHORE; DIOXIDE; IMPACT}},
Research-Areas = {{Oceanography}},
Web-of-Science-Categories  = {{Oceanography}},
Author-Email = {{wongcs@pac.dfo-mpo.gc.ca}},
ResearcherID-Numbers = {{Crawford, David W./AAS-9927-2020
   Crawford, David/B-5679-2012}},
ORCID-Numbers = {{Crawford, David W./0000-0003-2948-1007
   Crawford, David/0000-0003-2948-1007}},
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Number-of-Cited-References = {{38}},
Times-Cited = {{9}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{5}},
Journal-ISO = {{Deep-Sea Res. Part II-Top. Stud. Oceanogr.}},
Doc-Delivery-Number = {{611GP}},
Unique-ID = {{ISI:000179008300023}},
DA = {{2020-08-06}},
}

@article{ ISI:000173716100005,
Author = {Ferng, JJ},
Title = {{Toward a scenario analysis framework for energy footprints}},
Journal = {{ECOLOGICAL ECONOMICS}},
Year = {{2002}},
Volume = {{40}},
Number = {{1}},
Pages = {{53-69}},
Month = {{JAN}},
Abstract = {{There has been much improvement in calculation of the ecological
   footprint (EF) since 1996, when Wackernagel and Rees initially suggested
   it as a sustainable development index to evaluate human dependence on
   ecosystems in terms of land and water areas. However, despite the
   improvements the EF remains a static index, revealing only the current
   reality, so that it is criticized for its lack of use in policy
   formulation. This criticism is more concerned with the energy footprint
   because it dominates the estimated EF in many case studies, and its size
   would change almost simultaneously when alternative energy policies are
   implemented. One main reason for this deficiency is that the original
   calculation method does not explicitly take into account the linkages
   among the final consumption of goods and services, final energy
   consumption, and primary energy requirements. However, these linkages
   may contribute to scenarios and simulation of policy instruments for
   reducing energy footprints. This paper proposes a calculation framework
   to include the concerned linkages in order to: (1) estimate energy
   footprints according to the primary energies embodied in the goods and
   services consumed by a defined human population, and (2) develop
   scenarios and simulation of policy instruments for reducing energy
   footprints. This framework is then applied to Taiwan to illustrate how
   it works and what needs to be improved in future studies. (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 = {{Ferng, JJ (Corresponding Author), Natl Taipei Univ, Dept Land Econ \& Adm, 67,Sec 3,Ming Sheng E Rd, Taipei 10433, Taiwan.
   Natl Taipei Univ, Dept Land Econ \& Adm, Taipei 10433, Taiwan.}},
DOI = {{10.1016/S0921-8009(01)00270-1}},
ISSN = {{0921-8009}},
Keywords = {{energy footprint; scenario analysis; input-output analysis}},
Keywords-Plus = {{ECOLOGICAL FOOTPRINT; ENVIRONMENTAL-POLICY; METHODOLOGY; QUALITY; COST}},
Research-Areas = {{Environmental Sciences \& Ecology; Business \& Economics}},
Web-of-Science-Categories  = {{Ecology; Economics; Environmental Sciences; Environmental Studies}},
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   Yang JS, 1997, J NONDESTRUCT EVAL, V16, P1.}},
Number-of-Cited-References = {{26}},
Times-Cited = {{80}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{30}},
Journal-ISO = {{Ecol. Econ.}},
Doc-Delivery-Number = {{519GC}},
Unique-ID = {{ISI:000173716100005}},
DA = {{2020-08-06}},
}

@article{ ISI:000178884200013,
Author = {Ichiyanagi, K and Numaguti, A and Kato, K},
Title = {{Interannual variation of stable isotopes in Antarctic precipitation in
   response to El Nino-Southern Oscillation}},
Journal = {{GEOPHYSICAL RESEARCH LETTERS}},
Year = {{2002}},
Volume = {{29}},
Number = {{1}},
Month = {{JAN 1}},
Abstract = {{{[}1] Evidence for a close relationship between the interannual
   variation of stable isotopes in Antarctic precipitation and the El
   Nino-Southern Oscillation (ENSO) was found. Anomalies of sea surface
   temperature in the Equatorial Pacific and delta(18)O in precipitation in
   the Antarctic Peninsula are negatively correlated, both having a strong
   spectral power at about 3 years. The low (high) anomaly of delta(18)O is
   associated with southerly (northerly) and cold (warm) anomalies, which
   are considered appear as a response to the ENSO teleconnection. It was
   suggested that the flux and transport passway of southward moisture are
   the main factors determining the observed variation of stable isotopes
   in Antarctic precipitation.}},
Publisher = {{AMER GEOPHYSICAL UNION}},
Address = {{2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Ichiyanagi, K (Corresponding Author), Inst Global Change Res, Frontier Observ Res Syst Global Chenge, Kanazawa Ku, 3173-25 Showa Machi, Yokohama, Kanagawa 2360001, Japan.
   Inst Global Change Res, Frontier Observ Res Syst Global Chenge, Kanazawa Ku, Yokohama, Kanagawa 2360001, Japan.
   Nagoya Univ, Inst Hydrospher Atmospher Sci, Chikusa Ku, Nagoya, Aichi 4648601, Japan.
   Hokkaido Univ, Grad Sch Environm Earth Sci, Sapporo, Hokkaido 0600810, Japan.}},
DOI = {{10.1029/2000GL012815}},
Article-Number = {{1001}},
ISSN = {{0094-8276}},
EISSN = {{1944-8007}},
Keywords-Plus = {{SNOW}},
Research-Areas = {{Geology}},
Web-of-Science-Categories  = {{Geosciences, Multidisciplinary}},
Author-Email = {{kimpei@jamstec.go.jp
   numa@ees.hokudai.ac.jp
   kikukato@ihas.nagoya-u.ac.jp}},
Cited-References = {{BROMWICH DH, 1983, NATURE, V301, P145, DOI 10.1038/301145a0.
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   Renwick JA, 1999, MON WEATHER REV, V127, P2233, DOI 10.1175/1520-0493(1999)127<2233:BOTSPA>2.0.CO;2.
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   Yuan XJ, 2000, J CLIMATE, V13, P1697, DOI 10.1175/1520-0442(2000)013<1697:ASIEVA>2.0.CO;2.}},
Number-of-Cited-References = {{10}},
Times-Cited = {{13}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{4}},
Journal-ISO = {{Geophys. Res. Lett.}},
Doc-Delivery-Number = {{609CC}},
Unique-ID = {{ISI:000178884200013}},
DA = {{2020-08-06}},
}

@article{ ISI:000180975800017,
Author = {Ortlieb, L},
Title = {{Historical El Nino manifestations in South America since the sixteenth
   century}},
Journal = {{HOUILLE BLANCHE-REVUE INTERNATIONALE DE L EAU}},
Year = {{2002}},
Number = {{6-7}},
Pages = {{115-120}},
Abstract = {{A compilation of documentary data available for almost the last five
   centuries on climatic anomalies associated to El Nino in South America
   produced the reference sequence for the study of the ENSO system
   variability. Revisions of documentary information from Peru and Chile,
   as well as historical studies in northwestern Argentina and northeastern
   Brazil, indicated that this sequence of El Nino occurrences is less
   well-constrained that previously envisioned. The lack of synchronicity
   observed between manifestations of the phenomenon in several areas of
   the continent is puzzling and suggests that the teleconnection system
   varied through times. Actually, the reconstruction of the historical
   sequence of ENSO events should not yet be viewed as consolidated, and
   still requires a better understanding of the variability in space and
   time of the impacts of the phenomenon.}},
Publisher = {{EDP SCIENCES S A}},
Address = {{17, AVE DU HOGGAR, PA COURTABOEUF, BP 112, F-91944 LES ULIS CEDEX A,
   FRANCE}},
Type = {{Article}},
Language = {{French}},
Affiliation = {{Ortlieb, L (Corresponding Author), Inst Rech Dev, UR PALEOTROPIQUE 055, 32 Ave Henri Varagnat, F-93143 Bondy, France.
   Inst Rech Dev, UR PALEOTROPIQUE 055, F-93143 Bondy, France.}},
DOI = {{10.1051/lhb/2002094}},
ISSN = {{0018-6368}},
EISSN = {{1958-5551}},
Research-Areas = {{Water Resources}},
Web-of-Science-Categories  = {{Water Resources}},
ResearcherID-Numbers = {{ORTLIEB, Luc/A-8801-2011}},
Cited-References = {{Caviedes C.-N., 1973, P ASSOC AM GEOGR, V5, P44.
   CAVIEDES CN, 1991, FREIBURGER GEOGRAPHI, V32, P149.
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   SERRA A, 1973, ASPECTOS ESTATISTICO.}},
Number-of-Cited-References = {{18}},
Times-Cited = {{2}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{4}},
Journal-ISO = {{Houille Blanche-Rev. Int.}},
Doc-Delivery-Number = {{645KY}},
Unique-ID = {{ISI:000180975800017}},
DA = {{2020-08-06}},
}

@article{ ISI:000174663300006,
Author = {Matsuhashi, R and Kudoh, Y and Yoshida, Y and Ishitani, H and Yoshioka,
   M and Yoshioka, K},
Title = {{Life cycle of CO2-emissions from electric vehicles and gasoline vehicles
   utilizing a process-relational model}},
Journal = {{INTERNATIONAL JOURNAL OF LIFE CYCLE ASSESSMENT}},
Year = {{2002}},
Volume = {{7}},
Number = {{2}},
Pages = {{93-94}},
Abstract = {{This article aims at estimating life cycle CO2 emissions from electric
   vehicles (EV) and gasoline vehicles (GV), although the estimation in
   this study is not an LCA according to ISO14040s. For this purpose, a
   mathematical tool called the Process-relational model was developed. The
   Process-relational model is used for establishing lifecycle inventories.
   The model has a structure which improved the principle of input-output
   analysis in econometrics that only one product is generated by one
   process. This model enabled us to overcome difficulties of LCA in
   retracing complicated repercussions among production systems.
   Then, life cycle CO2 emissions from electric vehicles (EV) and gasoline
   vehicles (GV) were estimated with this model. Estimated results
   indicated that the manufacture and driving of EV resulted in less CO2
   emissions than those of GV. However, the difference between EV and GV
   dramatically changed depending on traffic situations. Namely, the
   difference became larger as the average velocity of the vehicles became
   lower. We also compared CO2 emission from manufacturing EV with that
   from driving EV. The share of manufacture was shown to increase in total
   CO2 emissions as the average velocity of the EV became higher.
   In conclusion, we clarified the direction of research and development of
   EV and GV for reducing the life cycle CO2.}},
Publisher = {{ECOMED PUBLISHERS}},
Address = {{RUDOLF-DIESEL-STR 3, D-86899 LANDSBERG, GERMANY}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Matsuhashi, R (Corresponding Author), Univ Tokyo, Fac Engn, Dept Geosyst Engn, Bunkyo Ku, Hongo 7-3-1, Tokyo 1138656, Japan.
   Univ Tokyo, Fac Engn, Dept Geosyst Engn, Bunkyo Ku, Tokyo 1138656, Japan.
   Univ Osaka Prefecture, Coll Engn, Dept Comp \& Syst Sci, Sakai, Osaka 5998231, Japan.
   Keio Univ, Keio Econ Observ, Minato Ku, Tokyo 1088345, Japan.}},
DOI = {{10.1065/lca2000.04.027}},
ISSN = {{0948-3349}},
Research-Areas = {{Engineering; Environmental Sciences \& Ecology}},
Web-of-Science-Categories  = {{Engineering, Environmental; Environmental Sciences}},
ResearcherID-Numbers = {{Kudoh, Yuki/L-6870-2018}},
ORCID-Numbers = {{Kudoh, Yuki/0000-0001-8408-4763}},
Number-of-Cited-References = {{0}},
Times-Cited = {{0}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{13}},
Journal-ISO = {{Int. J. Life Cycle Assess.}},
Doc-Delivery-Number = {{535TW}},
Unique-ID = {{ISI:000174663300006}},
DA = {{2020-08-06}},
}

@article{ ISI:000175876600003,
Author = {Suh, S and Huppes, G},
Title = {{Missing Inventory Estimation Tool using extended Input-Output Analysis}},
Journal = {{INTERNATIONAL JOURNAL OF LIFE CYCLE ASSESSMENT}},
Year = {{2002}},
Volume = {{7}},
Number = {{3}},
Pages = {{134-140}},
Abstract = {{Intention, Goal, Scope, Background: Input-Output Analysis (IOA) has
   recently been introduced to Life Cycle Assessment (LCA). In applying IOA
   to LCA studies, however, it is important to note that there are both
   advantages and disadvantages.
   Objectives: This paper aims to provide a better understanding of the
   advantages and disadvantages of adopting IOA in LCA, and introduces the
   methodology and principles of the Missing Inventory Estimation Tool
   (MIET) as one of the approaches to combine the strengths of
   process-specific LCA and IOA. Additionally, we try to identify a number
   of possible errors in the use of IOA for LCA purposes, due to confusion
   between industry output and commodity, consumer's price and producer's
   price.
   Method: MIET utilises the 1996 US input-output table and various
   environmental statistics. It is based on an explicit distinction between
   commodity and industry output.
   Results and Discussion: MIET is a self-contained, publicly available
   database which can be applied directly in LCA studies to estimate
   missing processes.
   Conclusion: By adopting MIET results in existing, process-based,
   life-cycle inventory (LCI), LCA practitioners can fully utilise the
   process-specific information while expanding the system boundary.
   Recommendations and Outlook: MIET will be continuously updated to
   reflect both methodological developments and newly available data
   sources. For supporting information see
   http://www.leidenuniv.nl/cml/ssp/software/miet.}},
Publisher = {{SPRINGER HEIDELBERG}},
Address = {{TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Suh, S (Corresponding Author), Leiden Univ, Ctr Environm Sci, CML, POB 9518, NL-2300 RA Leiden, Netherlands.
   Leiden Univ, Ctr Environm Sci, CML, NL-2300 RA Leiden, Netherlands.}},
DOI = {{10.1007/BF02994047}},
ISSN = {{0948-3349}},
EISSN = {{1614-7502}},
Keywords = {{cut-off; Input-Output Analysis (IOA); LCI; Missing Inventory Estimation
   Tool (MIET)}},
Research-Areas = {{Engineering; Environmental Sciences \& Ecology}},
Web-of-Science-Categories  = {{Engineering, Environmental; Environmental Sciences}},
Author-Email = {{suh@cml.leidenuniv.nl}},
ResearcherID-Numbers = {{Suh, Sangwon/E-2019-2011}},
ORCID-Numbers = {{Suh, Sangwon/0000-0001-8290-6276}},
Cited-References = {{{[}Anonymous], 1998, 14041 ISO.
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Number-of-Cited-References = {{43}},
Times-Cited = {{108}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{22}},
Journal-ISO = {{Int. J. Life Cycle Assess.}},
Doc-Delivery-Number = {{556YF}},
Unique-ID = {{ISI:000175876600003}},
DA = {{2020-08-06}},
}

@article{ ISI:000175063500005,
Author = {Kitzberger, T},
Title = {{ENSO as a forewarning tool of regional fire occurrence in northern
   Patagonia, Argentina}},
Journal = {{INTERNATIONAL JOURNAL OF WILDLAND FIRE}},
Year = {{2002}},
Volume = {{11}},
Number = {{1}},
Pages = {{33-39}},
Abstract = {{Composite series of ENSO indices recorded over 36 months preceding major
   fire years in four National Parks in northern Patagonia were compared
   with series of these indices for individual years over the period
   1950-1996 by means of an additive temporal phase coherence index.
   Logistic regressions of the dichotomous variable high vs low regional
   fire occurrence against the coherence index gained highest significant
   classificatory power using an index based on SST anomaly data between
   January of year -3 to August of year -1, Thus, warnings of extreme fire
   seasons could be declared as early as 3 months before the full fire
   season starts (i.e. early September). A regional fire season readiness
   index is proposed based on the periodicity of the Southern Oscillation,
   strong links with climate at particular regions of the globe, and
   empirically derived climatic controls on fine fuel buildup and coarse
   fuel desiccation. This long-range alerting tool could help
   decision-makers prepare preventative measures to mitigate the effects of
   large, high intensity wildfire seasons. However, it should be used with
   caution given that differences in timing in the onset of ENSO events and
   instability in teleconnection patterns could change climatic sequences,
   differentially affecting fire susceptibility.}},
Publisher = {{C S I R O PUBLISHING}},
Address = {{150 OXFORD ST, PO BOX 1139, COLLINGWOOD, VICTORIA 3066, AUSTRALIA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Kitzberger, T (Corresponding Author), Univ Nacl Comahue, Dept Ecol, Lab Ecotono, Quintral 1250, RA-8400 San Carlos De Bariloche, Rio Negro, Argentina.
   Univ Nacl Comahue, Dept Ecol, Lab Ecotono, RA-8400 San Carlos De Bariloche, Rio Negro, Argentina.}},
DOI = {{10.1071/WF01041}},
ISSN = {{1049-8001}},
Keywords = {{ENSO; regional fire occurrence; El Nino; forecasting; Patagonia}},
Keywords-Plus = {{FOREST-STEPPE ECOTONE; SOUTHERN OSCILLATION; CLIMATIC VARIABILITY;
   TREE-RING; HISTORY; DISTURBANCE; HUMANS}},
Research-Areas = {{Forestry}},
Web-of-Science-Categories  = {{Forestry}},
ResearcherID-Numbers = {{Kitzberger, Thomas/H-9209-2015}},
ORCID-Numbers = {{Kitzberger, Thomas/0000-0002-9754-4121}},
Cited-References = {{ACEITUNO P, 1988, MON WEATHER REV, V116, P505, DOI 10.1175/1520-0493(1988)116<0505:OTFOTS>2.0.CO;2.
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Number-of-Cited-References = {{25}},
Times-Cited = {{19}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{3}},
Journal-ISO = {{Int. J. Wildland Fire}},
Doc-Delivery-Number = {{542UW}},
Unique-ID = {{ISI:000175063500005}},
DA = {{2020-08-06}},
}

@article{ ISI:000173967300001,
Author = {Volodin, EM},
Title = {{Numerical coupled model for the global atmosphere and the tropical
   Pacific}},
Journal = {{IZVESTIYA ATMOSPHERIC AND OCEANIC PHYSICS}},
Year = {{2002}},
Volume = {{38}},
Number = {{1}},
Pages = {{1-14}},
Month = {{JAN-FEB}},
Abstract = {{The climate produced in a 20-year integration of a coupled model for the
   general atmospheric circulation and the tropical Pacific is analyzed.
   The error in the simulated annual mean sea surface temperature (SST) is
   less than 1.5 degrees almost everywhere in the computational domain. The
   basic features of the observed distribution of the mixed layer depth and
   the structure and velocities of tropical currents are well reproduced by
   the model. The interannual variability of the model SST is similar to
   the observed variability in the central Pacific and is smaller than the
   observed variability near the eastern coast. The time variability of the
   model SST, with a dominant period of 2.5 years, is more regular than the
   observed variability. The simulated anomalies in the mixed layer depth
   and the lower tropospheric wind during El Nino events are close in value
   to observed anomalies. The teleconnection response of the atmospheric
   dynamics to El Nino is similar in structure to the observed response but
   has a somewhat smaller value.}},
Publisher = {{MAIK NAUKA/INTERPERIODICA/SPRINGER}},
Address = {{233 SPRING ST, NEW YORK, NY 10013-1578 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Volodin, EM (Corresponding Author), Russian Acad Sci, Inst Numer Math, Ul Gubkina 8, Moscow 117930, Russia.
   Russian Acad Sci, Inst Numer Math, Moscow 117930, Russia.}},
ISSN = {{0001-4338}},
EISSN = {{1555-628X}},
Keywords-Plus = {{GENERAL-CIRCULATION MODEL; VARIABILITY; CLIMATE}},
Research-Areas = {{Meteorology \& Atmospheric Sciences; Oceanography}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences; Oceanography}},
Author-Email = {{volodin@inm.ras.ru}},
ResearcherID-Numbers = {{\\volodin, Evgeny/F-9571-2013}},
Cited-References = {{ALEKSEEV VA, 1988, 2086B98 RUSS AC SCI.
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Number-of-Cited-References = {{18}},
Times-Cited = {{1}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{0}},
Journal-ISO = {{Izv. Atmos. Ocean. Phys.}},
Doc-Delivery-Number = {{523QW}},
Unique-ID = {{ISI:000173967300001}},
DA = {{2020-08-06}},
}

@article{ ISI:000177170100002,
Author = {Lenzen, M},
Title = {{A guide for compiling inventories in hybrid life-cycle assessments: some
   Australian results}},
Journal = {{JOURNAL OF CLEANER PRODUCTION}},
Year = {{2002}},
Volume = {{10}},
Number = {{6}},
Pages = {{545-572}},
Abstract = {{Hybrid life-cycle assessment employing input-output analysis has
   advantages over conventional methods. In the inventory phase of a hybrid
   assessment. the data collection and the boundary selection can be
   tailored by using structural path analysis. This technique was applied
   to recent Australian data in order to determine environmentally
   important input paths in terms of energy consumption. land disturbance,
   beater use. and emissions of greenhouse gases, NOx, and SO2, for all
   Australian industry sectors. Due to the complexity of inter-industrial
   transactions, up to third-order paths can be top-ranking. The
   identification of such paths is considerably more labour-intensive in
   conventional life-cycle assessments. (C) 2002 Elsevier Science Ltd. All
   rights reserved.}},
Publisher = {{ELSEVIER SCI LTD}},
Address = {{THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Lenzen, M (Corresponding Author), Univ Sydney, Dept Appl Phys, A28, Sydney, NSW 2006, Australia.
   Univ Sydney, Dept Appl Phys, Sydney, NSW 2006, Australia.}},
DOI = {{10.1016/S0959-6526(02)00007-0}},
Article-Number = {{PII S0959-6526(01)00007-0}},
ISSN = {{0959-6526}},
EISSN = {{1879-1786}},
Keywords = {{hybrid LCA; structural path analysis; input-output analysis; Australia}},
Keywords-Plus = {{INPUT-OUTPUT-ANALYSIS; ENERGY; ERROR}},
Research-Areas = {{Science \& Technology - Other Topics; Engineering; Environmental
   Sciences \& Ecology}},
Web-of-Science-Categories  = {{Green \& Sustainable Science \& Technology; Engineering, Environmental;
   Environmental Sciences}},
Author-Email = {{m.lenzen@physics.usyd.edu.au}},
ResearcherID-Numbers = {{Lenzen, Manfred/D-3161-2013
   }},
ORCID-Numbers = {{Lenzen, Manfred/0000-0002-0828-5288}},
Cited-References = {{{*}AS NZS ISO, 1999, 140411999 ASNZS ISO.
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Number-of-Cited-References = {{41}},
Times-Cited = {{106}},
Usage-Count-Last-180-days = {{3}},
Usage-Count-Since-2013 = {{35}},
Journal-ISO = {{J. Clean Prod.}},
Doc-Delivery-Number = {{579GK}},
Unique-ID = {{ISI:000177170100002}},
DA = {{2020-08-06}},
}

@article{ ISI:000173256600006,
Author = {Yang, S and Lau, KM and Kim, KM},
Title = {{Variations of the East Asian jet stream and Asian-Pacific-American
   winter climate anomalies}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2002}},
Volume = {{15}},
Number = {{3}},
Pages = {{306-325}},
Abstract = {{In this study, the authors apply the NCEP-NCAR reanalysis and other
   observations to depict the association of the Asian-Pacific-American
   climate with the East Asian jet stream (EAJS). With an emphasis on
   boreal winter seasons and on interannual timescales, they analyze the
   variations of the EAJS and their relationships with El Nino-Southern
   Oscillation (ENSO) and extratropical North Pacific sea surface
   temperature (SST), and assess the relative connections of the EAJS and
   ENSO to the anomalies of atmospheric circulation, surface temperature,
   and precipitation in the Asian-Pacific-American region.
   It is found that the EAJS is coupled to a teleconnection pattern
   spanning the entire Asian-Pacific-American region with the strongest
   signals over east Asia and the western Pacific. This pattern differs
   significantly from that associated with ENSO, which influences the
   earth's climate extensively with a strongest impact on the climate over
   the central Pacific and east. A strong EAJS is associated with an
   intensification of the weather and climate systems in Asia and over the
   Pacific such as deepening of the east Asian trough and the Aleutian low
   and strengthening of the east Asian winter monsoon. It is linked to
   colder and drier conditions in east Asia and stronger convection over
   the tropical Asia-Australia sector. Compared with ENSO, the EAJS seems
   to link to the climate signals of Asia and the Pacific more strongly. An
   intensified EAJS is also associated with anomalies of temperature and
   precipitation in North America due to the related changes in stationary
   wave patterns.
   While the EAJS does not strongly link to the tropical central-eastern
   Pacific SST, it is significantly associated with the extratropical North
   Pacific SST, more specifically the second most dominant mode of the
   empirical orthogonal function analysis of the SST. In addition, a strong
   (weak) EAJS seems to follow a large (small) meridional gradient of the
   western Pacific SST associated with warming (cooling) in the
   Tropics-subtropics and cooling (warming) in the extratropics.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Yang, S (Corresponding Author), NOAA, NWS, NCEP Climate Predict Ctr, 5200 Auth Rd,Room 605, Camp Springs, MD 20746 USA.
   NOAA, NWS, NCEP Climate Predict Ctr, Camp Springs, MD 20746 USA.
   NASA, Atmospheres Lab, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA.
   Sci Syst \& Applicat Inc, Lanham, MD USA.}},
DOI = {{10.1175/1520-0442(2002)015<0306:VOTEAJ>2.0.CO;2}},
ISSN = {{0894-8755}},
EISSN = {{1520-0442}},
Keywords-Plus = {{SEA-SURFACE-TEMPERATURE; EXTRATROPICAL SST ANOMALIES;
   GENERAL-CIRCULATION MODEL; SUMMER MONSOON; NORTH PACIFIC; ATMOSPHERIC
   RESPONSE; EL-NINO; TROPICAL PACIFIC; STATIONARY WAVES; 3-DIMENSIONAL
   PROPAGATION}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{song.yang@noaa.gov}},
ResearcherID-Numbers = {{Kim, Kyu-Myong/G-5398-2014
   Yang, Song/B-4952-2009
   Lau, William K/E-1510-2012}},
ORCID-Numbers = {{Lau, William K/0000-0002-3587-3691}},
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