text:
Although the slow patterns and the
   total patterns look similar, they have some important differences. The
   slow patterns are more closely related to the slowly varying external
   forcing and very low-frequency internal dynamics than those derived by
   the sample covariance matrix. This is evidenced by the fact that the
   principal component time series of the slow patterns have a larger
   proportion of variability related to these factors. Where tropical SST
   forcing is important, the slow patterns tended to be more highly
   correlated with the interannual variations in the forcing. Three slow
   modes, related to the Tropical Northern Hemisphere, East Atlantic and
   Western Pacific teleconnections, are all significantly related to
   tropical SST variability associated predominantly with the El
   Nino-Southern Oscillation, in the case of the first two, and Indian
   Ocean variability, in the third case. The derived slow patterns and
   intraseasonal patterns may help to better understand the long-range
   predictability, uncertainty, and forcing of climate variables, for the
   wintertime circulation.}},
Publisher = {{SPRINGER}},
Address = {{233 SPRING ST, NEW YORK, NY 10013 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Frederiksen, CS (Corresponding Author), Bur Meteorol Res Ctr, GPO Box 1289, Melbourne, Vic 3001, Australia.
   Bur Meteorol Res Ctr, Melbourne, Vic 3001, Australia.
   Natl Inst Water \& Atmospher Res, Wellington, New Zealand.}},
DOI = {{10.1007/s00382-004-0429-6}},
ISSN = {{0930-7575}},
EISSN = {{1432-0894}},
Keywords-Plus = {{SEA-LEVEL PRESSURE; 3-DIMENSIONAL INSTABILITY THEORY; EXTRATROPICAL SST
   ANOMALIES; NORTHERN-HEMISPHERE WINTER; TELECONNECTION PATTERNS;
   GEOPOTENTIAL HEIGHT; GLOBAL ATMOSPHERE; TROPICAL PACIFIC; LINEAR-THEORY;
   STORM TRACKS}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{C.Frederiksen@bom.gov.au}},
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Number-of-Cited-References = {{44}},
Times-Cited = {{23}},
Usage-Count-Last-180-days = {{1}},
Usage-Count-Since-2013 = {{6}},
Journal-ISO = {{Clim. Dyn.}},
Doc-Delivery-Number = {{851WK}},
Unique-ID = {{ISI:000223717000007}},
DA = {{2020-08-06}},
}

@article{ ISI:000222198600011,
Author = {Schacter, J and Thum, YM},
Title = {{Paying for high- and low-quality teaching}},
Journal = {{ECONOMICS OF EDUCATION REVIEW}},
Year = {{2004}},
Volume = {{23}},
Number = {{4}},
Pages = {{411-430}},
Month = {{AUG}},
Abstract = {{The extensive research on teacher quality has led to two conclusions.
   First, there are large and significant differences among teachers in
   terms of their capacity to improve student achievement. Second, these
   differences are hot captured by common measures of teacher
   qualifications (E.A. Hanushek, Teacher quality, in: L.T. Izumi, W.M.
   Evers (Eds.), Teacher Quality, Hoover Press, Palo Alto, CA, 2002, pp.
   1-12). We present the argument that in order to improve teacher quality,
   one must focus on teacher performance. By creating teaching standards
   and performance rubrics, rating teachers against those standards, and
   then employing a multivariate multilevel mixed statistical model to
   attribute students' achievement gains to teachers, we both designed and
   provided preliminary validation evidence for a system to judge teachers
   based on performance. Our results demonstrate that teaching performance
   as defined by our standards and rubrics is highly predictive of student
   academic progress across the elementary grades. Implications for our
   research to improve teaching through implementing performance pay
   systems are discussed. (C) 2003 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 = {{Schacter, J (Corresponding Author), Milken Family Fdn, 1250 4th St, Santa Monica, CA 90401 USA.
   Milken Family Fdn, Santa Monica, CA 90401 USA.
   Univ Calif Los Angeles, Grad Sch Educ, Los Angeles, CA 90095 USA.}},
DOI = {{10.1016/j.econedurev.2003.08.002}},
ISSN = {{0272-7757}},
Keywords = {{teacher salaries; input output analysis; productivity; salary wage
   differentials}},
Keywords-Plus = {{SCHOOL RESOURCES; ACHIEVEMENT; MOTIVATION; CLASSROOM; FOUNDATIONS;
   KNOWLEDGE; SCIENCE; MODEL; GOAL}},
Research-Areas = {{Business \& Economics; Education \& Educational Research}},
Web-of-Science-Categories  = {{Economics; Education \& Educational Research}},
Author-Email = {{schacter@sbcglobal.net}},
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Number-of-Cited-References = {{50}},
Times-Cited = {{46}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{20}},
Journal-ISO = {{Econ. Educ. Rev.}},
Doc-Delivery-Number = {{831MN}},
Unique-ID = {{ISI:000222198600011}},
DA = {{2020-08-06}},
}

@article{ ISI:000222305600008,
Author = {Brulhart, M and Trionfetti, F},
Title = {{Public expenditure, international specialisation and agglomeration}},
Journal = {{EUROPEAN ECONOMIC REVIEW}},
Year = {{2004}},
Volume = {{48}},
Number = {{4}},
Pages = {{851-881}},
Month = {{AUG}},
Abstract = {{It is widely recognised that public-sector purchasers tend to favour
   domestic suppliers. We study the consequences of such home-biased public
   procurement on international specialisation. Using a general-equilibrium
   model with a monopolistically competitive sector, we find that a country
   will specialise in that sector if it has relatively large home-biased
   procurement (the ``pull{''} effect). Furthermore, home-biased
   procurement can counter agglomeration forces in that sector and thereby
   attenuate the overall degree of international specialisation (the
   ``spread{''} effect). Our empirical analysis, conducted on input-output
   data for the European Union, yields supporting evidence for the pull
   effect and some support for the spread effect. (C) 2003 Elsevier B.V.
   All rights reserved.}},
Publisher = {{ELSEVIER SCIENCE BV}},
Address = {{PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Brulhart, M (Corresponding Author), Univ Lausanne, Ecole HEC, Dept Economet \& Econ Polit, CH-1015 Lausanne, Switzerland.
   Univ Lausanne, Ecole HEC, Dept Economet \& Econ Polit, CH-1015 Lausanne, Switzerland.
   Univ Paris 13, CNRS, CEPN, F-75015 Paris, France.
   CEP11, F-75015 Paris, France.}},
DOI = {{10.1016/j.euroecorev.2003.09.002}},
ISSN = {{0014-2921}},
Keywords = {{public expenditure; international specialisation; economic geography;
   European Union; input-output analysis}},
Keywords-Plus = {{GOVERNMENT PROCUREMENT; GEOGRAPHY; POLICY; TRADE}},
Research-Areas = {{Business \& Economics}},
Web-of-Science-Categories  = {{Economics}},
Author-Email = {{marius.brulhart@hec.unil.ch
   trionfetti@seg.univ-paris13.fr}},
ResearcherID-Numbers = {{Brulhart, Marius/B-8633-2008
   }},
ORCID-Numbers = {{Brulhart, Marius/0000-0001-5483-0219}},
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Number-of-Cited-References = {{28}},
Times-Cited = {{38}},
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Usage-Count-Since-2013 = {{5}},
Journal-ISO = {{Eur. Econ. Rev.}},
Doc-Delivery-Number = {{832ZG}},
Unique-ID = {{ISI:000222305600008}},
DA = {{2020-08-06}},
}

@article{ ISI:000223052600011,
Author = {Veski, S and Seppa, H and Ojala, AEK},
Title = {{Cold event at 8200 yr BP recorded in annually laminated lake sediments
   in eastern Europe}},
Journal = {{GEOLOGY}},
Year = {{2004}},
Volume = {{32}},
Number = {{8}},
Pages = {{681-684}},
Month = {{AUG}},
Abstract = {{A quantitative annual mean temperature reconstruction from an annually
   laminated lake-sediment sequence in Estonia, eastern Europe, shows a
   distinct cold period at 84008080 yr B.P. (= before A.D. 2000); the
   timing is consistent with that seen in the Greenland ice-core data and
   various high-resolution records from western Europe. During maximal
   cooling at 8250-8150 yr B.P., the annual mean temperature in Estonia was
   similar to2.0 degreesC colder than prior to and similar to3.0 degreesC
   colder than after the cooling. The pollen-stratigraphic and
   sedimentological data suggest especially cold and snowy winter
   conditions. The duration and amplitude of the cold event agree with the
   modeled impact of a sudden freshening of the North Atlantic surface
   water and subsequent perturbation of the thermohaline circulation.
   Provided that the cold event was caused by a pulse of freshwater-from
   the melting Laurentide Ice Sheet-to the North Atlantic, the results
   indicate a strong teleconnection between the North Atlantic oceanic
   forcing and the east European climate at least up to long 26degreesE,
   mediated probably by the changing intensity of the zonal atmospheric
   circulation.}},
Publisher = {{GEOLOGICAL SOC AMER, INC}},
Address = {{PO BOX 9140, BOULDER, CO 80301-9140 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Veski, S (Corresponding Author), Tallinn Univ Technol, Inst Geol, Estonia Pst 7, EE-10143 Tallinn, Estonia.
   Tallinn Univ Technol, Inst Geol, EE-10143 Tallinn, Estonia.
   Univ Helsinki, Dept Geol, FIN-00014 Helsinki, Finland.
   Geol Survey Finland, FIN-02150 Espoo, Finland.}},
DOI = {{10.1130/G20683.1}},
ISSN = {{0091-7613}},
EISSN = {{1943-2682}},
Keywords = {{varve chronology; pollen; oxygen isotopes; 8200 yr B.P cold event;
   thermohaline circulation; Estonia}},
Keywords-Plus = {{ABRUPT CLIMATE-CHANGE; NORTH-ATLANTIC CLIMATE; OXYGEN-ISOTOPE;
   ATMOSPHERIC CIRCULATION; LACUSTRINE CARBONATES; HOLOCENE CHANGES; OCEAN;
   VARIABILITY; OSCILLATION; IMPACTS}},
Research-Areas = {{Geology}},
Web-of-Science-Categories  = {{Geology}},
Author-Email = {{Veski@gi.ee
   heikki.seppa@helsinki.fi
   antti.ojala@gsf.fi}},
ResearcherID-Numbers = {{Veski, Siim/A-9417-2014}},
ORCID-Numbers = {{Veski, Siim/0000-0002-8297-2385}},
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Number-of-Cited-References = {{33}},
Times-Cited = {{105}},
Usage-Count-Last-180-days = {{2}},
Usage-Count-Since-2013 = {{22}},
Journal-ISO = {{Geology}},
Doc-Delivery-Number = {{843CH}},
Unique-ID = {{ISI:000223052600011}},
DA = {{2020-08-06}},
}

@article{ ISI:000223985000002,
Author = {Last, M and Friedman, M and Kandel, A},
Title = {{Using data mining for Automated Software Testing}},
Journal = {{INTERNATIONAL JOURNAL OF SOFTWARE ENGINEERING AND KNOWLEDGE ENGINEERING}},
Year = {{2004}},
Volume = {{14}},
Number = {{4}},
Pages = {{369-393}},
Month = {{AUG}},
Note = {{15th International Conference on Software Engineering and Knowledge
   Engineering, San Francisco, CA, JUL 01-03, 2003}},
Abstract = {{In today's software industry, the design of test cases is mostly based
   on human expertise, while test automation tools are limited to execution
   of pre-planned tests only. Evaluation of test outcomes is also
   associated with a considerable effort by human testers who often have
   imperfect knowledge of the requirements specification. Not surprisingly,
   this manual approach to software testing results in heavy losses to the
   world's economy. In this paper, we demonstrate the potential use of data
   mining algorithms for automated modeling of tested systems. The data
   mining models can be utilized for recovering system requirements,
   designing a minimal set of regression tests, and evaluating the
   correctness of software outputs. To study the feasibility of the
   proposed approach, we have applied a state-of-the-art data mining
   algorithm called Info-Fuzzy Network (IFN) to execution data of a complex
   mathematical package. The IFN method has shown a clear capability to
   identify faults in the tested program.}},
Publisher = {{WORLD SCIENTIFIC PUBL CO PTE LTD}},
Address = {{5 TOH TUCK LINK, SINGAPORE 596224, SINGAPORE}},
Type = {{Article; Proceedings Paper}},
Language = {{English}},
Affiliation = {{Last, M (Corresponding Author), Ben Gurion Univ Negev, Dept Informat Syst Engn, IL-84105 Beer Sheva, Israel.
   Nucl Res Ctr Negev, Dept Phys, IL-84190 Beer Sheva, Israel.
   Univ S Florida, Dept Comp Sci \& Engn, Tampa, FL 33620 USA.}},
DOI = {{10.1142/S0218194004001737}},
ISSN = {{0218-1940}},
EISSN = {{1793-6403}},
Keywords = {{Automated Software Testing; regression testing; input-output analysis;
   data mining; Info-Fuzzy Networks; finite element solver}},
Research-Areas = {{Computer Science; Engineering}},
Web-of-Science-Categories  = {{Computer Science, Artificial Intelligence; Computer Science, Software
   Engineering; Engineering, Electrical \& Electronic}},
Author-Email = {{mlast@bgumail.bgu.ac.il
   mlfrid@netvision.net.il
   kandel@csee.usf.edu}},
ResearcherID-Numbers = {{LAST, MARK/F-1424-2012
   Last, Mark/AAF-8443-2020}},
ORCID-Numbers = {{LAST, MARK/0000-0003-0748-7918
   }},
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Number-of-Cited-References = {{42}},
Times-Cited = {{18}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{2}},
Journal-ISO = {{Int. J. Softw. Eng. Knowl. Eng.}},
Doc-Delivery-Number = {{855PA}},
Unique-ID = {{ISI:000223985000002}},
DA = {{2020-08-06}},
}

@article{ ISI:000223074500007,
Author = {Fasullo, J},
Title = {{Biennial characteristics of Indian monsoon rainfall}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2004}},
Volume = {{17}},
Number = {{15}},
Pages = {{2972-2982}},
Month = {{AUG}},
Abstract = {{Basic diagnoses of summertime all-India rainfall ( AIR) are conducted in
   an effort to evaluate the hypothesis that asserts the biennial
   alternation between successive strong and weak Indian monsoon summer
   seasons. The associations between subsets of the 10, 20, and 30
   strongest and weakest monsoon seasons from 1871 to 2001, the mean
   rainfall in the summer seasons that precede and follow them, and the
   frequency with which the seasons are preceded or followed by strong
   (+10\%)/weak (-10\%) or surplus (above normal)/deficient (below normal)
   summer monsoon rainfall are assessed. The relationships are also
   stratified by the presence or absence of anomalous El Nino-Southern
   Oscillation (ENSO) conditions. Spectral and spatial comparisons between
   the monsoon's bienniality and ENSO teleconnection are then conducted
   using Indian district rainfall and wavelet decomposition.
   For the strongest monsoon seasons, statistically significant
   associations with the preceding summer rains are found that are
   consistent with the biennial hypothesis. In contrast, for years
   following the strongest monsoon seasons, and for years that both precede
   and follow the weakest monsoon seasons, significant biennial
   associations are largely absent. When the relationship with ENSO is
   considered, significant associations are found that act both in
   opposition to, and in support of, the biennial hypothesis. Often, strong
   La Nina seasons are preceded by weak or deficient summer rains, and weak
   El Nino seasons are followed by strong summer rains. The sequences
   identified are associated with transitions between El Nino and La Nina
   conditions. However, in contradiction to the biennial hypothesis, it is
   also found that following strong La Nina seasons, average monsoon
   rainfall lies significantly above its climatological average, and the
   frequencies with which both deficient and weak monsoon seasons occur are
   significantly below their expectation values.
   During years in which ENSO conditions are near neutral, evidence of
   bienniality is poor. Mean anomalies in summer rainfall preceding and
   following anomalous monsoon seasons during neutral ENSO conditions are
   either very weak or are not statistically discernable from chance. In
   addition, the frequency with which weak/neutral monsoon seasons are
   preceded by strong rains lies significantly below its expectation value,
   suggesting interannual persistence rather than bienniality. Only the
   frequency with which strong monsoon seasons are followed by deficient
   rains is found to be both statistically significant and consistent with
   the biennial hypothesis.
   Comparisons of the spectral and spatial characteristics of rainfall's
   bienniality and the correlation between rainfall and Nino-3 SST further
   illustrate the strong correspondence that exists between biennial
   monsoon variability and ENSO. The temporal evolution of biennial power
   in the monsoon is found to evolve closely with that of ENSO over the
   past 50 yr and the spatial distribution of bienniality in India is shown
   to mirror that of ENSO's teleconnection. The analysis suggests that
   theories attempting to describe the physical mechanisms that underlie
   monsoon bienniality must also begin to address the asymmetric and
   episodic nature of the monsoon's year-to-year variability. Moreover, the
   results bring into question the hypothesis that bienniality is an
   inherent mode of variability for a closed Indian Ocean-monsoon system.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Fasullo, J (Corresponding Author), Univ Colorado, Program Atmospher \& Ocean Sci, UCB-0311, Boulder, CO 80309 USA.
   Univ Colorado, Program Atmospher \& Ocean Sci, Boulder, CO 80309 USA.}},
DOI = {{10.1175/1520-0442(2004)017<2972:BCOIMR>2.0.CO;2}},
ISSN = {{0894-8755}},
Keywords-Plus = {{ASIAN SUMMER MONSOON; MRI COUPLED GCM; INTERANNUAL VARIABILITY; TROPICAL
   PACIFIC; OSCILLATION; OCEAN; SYSTEM; ENSO; PREDICTION; DYNAMICS}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{fasullo@colorado.edu}},
ResearcherID-Numbers = {{Fasullo, John/H-4552-2019}},
ORCID-Numbers = {{Fasullo, John/0000-0003-1216-892X}},
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Number-of-Cited-References = {{32}},
Times-Cited = {{24}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{7}},
Journal-ISO = {{J. Clim.}},
Doc-Delivery-Number = {{843JI}},
Unique-ID = {{ISI:000223074500007}},
DA = {{2020-08-06}},
}

@article{ ISI:000223074500012,
Author = {Wu, RG and Kirtman, BP},
Title = {{Impacts of the Indian Ocean on the Indian summer monsoon-ENSO
   relationship}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2004}},
Volume = {{17}},
Number = {{15}},
Pages = {{3037-3054}},
Month = {{AUG}},
Abstract = {{This study investigates the impacts of the Indian Ocean on the
   relationship between the Indian summer monsoon and the El Nino-Southern
   Oscillation (ENSO) through numerical simulations with a coupled
   atmosphere-ocean general circulation model and atmospheric general
   circulation model (AGCM) experiments with specified sea surface
   temperature (SST) and surface heat flux (SHF) forcing. Previous studies
   have shown that this particular coupled model captures many aspects of
   the observed Indian summer monsoon-ENSO relationship. However, it is
   found that, when the Indian Ocean is decoupled from the atmosphere, the
   Indian monsoon-ENSO relationship reverses. This change is linked to the
   relationships between surface evaporation, surface wind, and SST in the
   north Indian Ocean. In the coupled case, surface evaporation anomalies
   are positively correlated with surface wind anomalies during April-June
   and are of the same sign as SST anomalies during July-September. In the
   decoupled Indian Ocean case, surface evaporation anomalies are of the
   same sign as surface wind anomalies during the entire April-September
   period.
   Numerical experiments with an AGCM were performed with SST or SHF
   anomalies specified in the tropical Indian-Pacific Ocean, tropical
   Pacific Ocean only, and tropical Indian Ocean only. These experiments
   confirm the importance of local coupled air-sea feedback in the Indian
   Ocean for a proper simulation of the Indian monsoon-ENSO relationship.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Wu, RG (Corresponding Author), Ctr Ocean Land Atmosphere Studies, 4041 Powder Mill Rd,Suite 302, Calverton, MD 20705 USA.
   Ctr Ocean Land Atmosphere Studies, Calverton, MD 20705 USA.
   George Mason Univ, Sch Computat Sci, Fairfax, VA USA.}},
DOI = {{10.1175/1520-0442(2004)017<3037:IOTIOO>2.0.CO;2}},
ISSN = {{0894-8755}},
EISSN = {{1520-0442}},
Keywords-Plus = {{SEA-SURFACE-TEMPERATURE; TROPOSPHERIC BIENNIAL OSCILLATION;
   TROPICAL-WIDE TELECONNECTION; NINO-SOUTHERN-OSCILLATION;
   ASIAN-AUSTRALIAN MONSOON; EL-NINO; INTERANNUAL VARIATIONS; ARABIAN SEA;
   VARIABILITY; RAINFALL}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{renguang@cola.iges.org}},
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   Wang B, 2001, J CLIMATE, V14, P4073, DOI 10.1175/1520-0442(2001)014<4073:IVOTAS>2.0.CO;2.
   Wang B, 2003, J CLIMATE, V16, P1195, DOI 10.1175/1520-0442(2003)16\<1195:AOIAII\>2.0.CO;2.
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   Wu RG, 2004, J CLIMATE, V17, P1623, DOI 10.1175/1520-0442(2004)017\<1623:TTBOOT\>2.0.CO;2.
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   Yu LS, 1999, GEOPHYS RES LETT, V26, P735, DOI 10.1029/1999GL900072.}},
Number-of-Cited-References = {{54}},
Times-Cited = {{74}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{7}},
Journal-ISO = {{J. Clim.}},
Doc-Delivery-Number = {{843JI}},
Unique-ID = {{ISI:000223074500012}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000223257100009,
Author = {Assel, R and Drobot, S and Croley, TE},
Title = {{Improving 30-day Great Lakes ice cover outlooks}},
Journal = {{JOURNAL OF HYDROMETEOROLOGY}},
Year = {{2004}},
Volume = {{5}},
Number = {{4}},
Pages = {{713-717}},
Month = {{AUG}},
Abstract = {{Prediction of Great Lakes ice cover is important for winter operations
   and planning activities. Current 30-day forecasts use accumulated
   freezing degree-days (AFDDs) to identify similar historical events and
   associated ice cover. The authors describe statistical models that
   relate future ice cover to current ice cover, AFDDs, and teleconnection
   indices, available on the day the forecast is made. These models are
   evaluated through Monte Carlo simulation and assess the potential of a
   perfect AFDD forecast in a regression between ice cover and AFDDs
   between the forecast date (first day of month) and the date for which
   the forecast is made (first day of next month).}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Assel, R (Corresponding Author), NOAA, Great Lakes Environm Res Lab, 2205 Commonwealth Blvd, Ann Arbor, MI 48105 USA.
   NOAA, Great Lakes Environm Res Lab, Ann Arbor, MI 48105 USA.
   Natl Acad, Board Atmospher Sci \& Climate, Washington, DC USA.}},
DOI = {{10.1175/1525-7541(2004)005<0713:IDGLIC>2.0.CO;2}},
ISSN = {{1525-755X}},
EISSN = {{1525-7541}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{ray.assel@noaa.gov}},
Cited-References = {{Assel R, 1998, INT J CLIMATOL, V18, P425, DOI 10.1002/(SICI)1097-0088(19980330)18:4<425::AID-JOC258>3.3.CO;2-H.
   ASSEL RA, 2004, GLERL129 NOAA.
   ASSEL RA, 2003, GLERL127 NOAA.
   ASSEL RA, 2003, ELECT ATLAS GREAT LA.
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   SNIDER CR, 1974, 1 NOAA NWS OSD.
   Wilks DS, 1995, STAT METHODS ATMOSPH.}},
Number-of-Cited-References = {{8}},
Times-Cited = {{6}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{3}},
Journal-ISO = {{J. Hydrometeorol.}},
Doc-Delivery-Number = {{845PP}},
Unique-ID = {{ISI:000223257100009}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000223493100002,
Author = {Ciobanu, C and Mattas, K and Psaltopoulos, D},
Title = {{Structural changes in less developed areas: An input-output framework}},
Journal = {{REGIONAL STUDIES}},
Year = {{2004}},
Volume = {{38}},
Number = {{6}},
Pages = {{603-614}},
Month = {{AUG}},
Abstract = {{This paper uses an input-output framework to investigate structural
   changes within a time span of 17 years in the regional economy of East
   Macedonia and Thrace in North East Greece, which has gone through
   considerable changes after Greece's accession to the EU in 1981. The
   Generation of Regional Input-Output Tables procedure is followed for the
   construction of the relevant regional models. Then, changes in the
   structure of the regional economy are estimated using a series of
   indicators and structural decomposition analysis. Results reveal that
   between 1980 and 1997, the economy of the selected region has undergone
   significant transformations affecting both producing and consuming
   sectors. Also, final demand effects on gross production were more
   important than changes in technical coefficients, while employment
   requirements were significantly reduced. Finally, empirical findings
   provide an indication of the future trends in the structure of the
   regional economy.}},
Publisher = {{ROUTLEDGE JOURNALS, TAYLOR \& FRANCIS LTD}},
Address = {{2-4 PARK SQUARE, MILTON PARK, ABINGDON OX14 4RN, OXON, ENGLAND}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Ciobanu, C (Corresponding Author), Aristotle Univ Thessaloniki, Dept Agr Econ, POB 225, GR-54006 Thessaloniki, Greece.
   Aristotle Univ Thessaloniki, Dept Agr Econ, GR-54006 Thessaloniki, Greece.
   Univ Patras, Dept Econ, GR-26500 Patras, Greece.}},
DOI = {{10.1080/003434042000240914}},
ISSN = {{0034-3404}},
EISSN = {{1360-0591}},
Keywords = {{input-output analysis; changes; economic structure; region; indicators;
   agricultural sectors}},
Keywords-Plus = {{INDUSTRIALIZATION; ECONOMY; FOOD}},
Research-Areas = {{Business \& Economics; Environmental Sciences \& Ecology; Geography;
   Public Administration}},
Web-of-Science-Categories  = {{Economics; Environmental Studies; Geography; Regional \& Urban Planning}},
Author-Email = {{mattas@eng.auth.gr}},
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   GREEK EC.}},
Number-of-Cited-References = {{50}},
Times-Cited = {{8}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{13}},
Journal-ISO = {{Reg. Stud.}},
Doc-Delivery-Number = {{848UJ}},
Unique-ID = {{ISI:000223493100002}},
DA = {{2020-08-06}},
}

@article{ ISI:000222204200009,
Author = {Zhou, L and Grubbstrom, RW},
Title = {{Analysis of the effect of commonality in multi-level inventory systems
   applying MRP theory}},
Journal = {{INTERNATIONAL JOURNAL OF PRODUCTION ECONOMICS}},
Year = {{2004}},
Volume = {{90}},
Number = {{2}},
Pages = {{251-263}},
Month = {{JUL 28}},
Abstract = {{Commonality, i.e. using the same type of component in different
   locations of product structure trees, is frequently encountered in
   manufacturing industries. It has long been known that using a common
   component can reduce the cost of safety stock. Basically, taking
   commonality into account can reduce the inventory level, shorten the
   time for reaching the market, decrease the set-up time, increase
   productivity, and improve flexibility. However, using the same component
   in different locations might require that the component is made more
   flexible and, therefore, more expensive as compared to choosing
   tailor-made items for its respective locations. The manufacturing cost
   of commonality items may therefore be much higher because of its greater
   number of functions. So, there may be a balance to be struck between the
   value of the advantage of commonality, and the cost of its disadvantage.
   This paper focuses on the effect of commonality in multi-level
   production-inventory systems, especially assembly systems. The basic
   balance equations of MRP theory, using input output analysis together
   with the Laplace transform, are used for comparing the cases when
   commonality is disregarded, on the one hand, and when commonality is
   taken into account, on the other. Applying the net present value as the
   objective function, conclusions are derived in the form of conditions
   for when commonality is recommended, and when not. (C) 2003 Elsevier
   B.V. All rights reserved.}},
Publisher = {{ELSEVIER SCIENCE BV}},
Address = {{PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Zhou, L (Corresponding Author), Linkoping Inst Technol, Dept Prod Econ, S-58183 Linkoping, Sweden.
   Linkoping Inst Technol, Dept Prod Econ, S-58183 Linkoping, Sweden.
   Nanchang Univ, Automat Inst, Nanchang 330029, Jiangxi, Peoples R China.}},
DOI = {{10.1016/S0925-5273(03)00208-1}},
ISSN = {{0925-5273}},
EISSN = {{1873-7579}},
Keywords = {{commonality; prod action; inventory system Material requirements
   planning (MRP); input-output analysis; Laplace transform}},
Keywords-Plus = {{COMPONENT PART COMMONALITY; SAFETY STOCK LEVELS; MULTIPLE-PERIOD; MODEL;
   COSTS}},
Research-Areas = {{Engineering; Operations Research \& Management Science}},
Web-of-Science-Categories  = {{Engineering, Industrial; Engineering, Manufacturing; Operations Research
   \& Management Science}},
Author-Email = {{zl6357@vip.sina.com
   rwg@ipe.liu.se}},
Cited-References = {{BAKER KR, 1986, MANAGE SCI, V32, P982, DOI 10.1287/mnsc.32.8.982.
   BAKER KR, 1985, J OPERATIONS MANAGEM, V6, P13.
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   MCCLAIN JO, 1984, MANAGE SCI, V30, P772, DOI 10.1287/mnsc.30.6.772.
   MOLINA A, 1995, P WORK C REENG ENT I, P11.}},
Number-of-Cited-References = {{13}},
Times-Cited = {{21}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{7}},
Journal-ISO = {{Int. J. Prod. Econ.}},
Doc-Delivery-Number = {{831ON}},
Unique-ID = {{ISI:000222204200009}},
DA = {{2020-08-06}},
}

@article{ ISI:000223504500005,
Author = {Wu, MD and Xu, LH and Weng, D},
Title = {{The NO selective reduction on the La-1-xSrxMnO3 catalysts}},
Journal = {{CATALYSIS TODAY}},
Year = {{2004}},
Volume = {{90}},
Number = {{3-4}},
Pages = {{199-206}},
Month = {{JUL 1}},
Note = {{1st China/Japan Workshop on Environmental Catalysis and Eco-Materials,
   Beijing, PEOPLES R CHINA, OCT 07-10, 2003}},
Organization = {{Natl Nat Sci Fdn China; Chinese Acad Sci}},
Abstract = {{La1-xSrxMnO3 (x = 0, 0.1, 0.3, 0.5, 0.7) perovskite-type oxides (PTOs)
   were prepared by coprecipitation under various calcination temperature,
   and their performances for the NO reduction were evaluated under a
   simulated exhaust gas mixture. The X-ray diffraction (XRD) and
   thermogravimetric analysis were carried out to find the formation
   process of the perovskite. The NO reduction rate under different
   reaction temperature, the concentration of oxygen and the presence of
   hydrocarbon were observed by the input/output analysis. In the presence
   of 10\% excess oxygen, the catalyst La0.7Sr0.3MnO3 calcined at
   900degreesC showed a NO reduction rate of 61\% at 380degreesC. The study
   of the reaction curves showed that C3H8 could act as the reducer for the
   NO reduction below 400degreesC. The NO reduction is highly affected by
   increasing the O-2 concentration from 0.5 to 10\%, especially at high
   temperatures when oxygen becomes more competitive than NO on the
   oxidation of C3H8, leading to a decrease of the NO reduction from 100\%
   to zero at 560degreesC. (C) 2004 Elsevier B.V. All rights reserved.}},
Publisher = {{ELSEVIER SCIENCE BV}},
Address = {{PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS}},
Type = {{Article; Proceedings Paper}},
Language = {{English}},
Affiliation = {{Wu, MD (Corresponding Author), Tsing Hua Univ, Dept Mat Sci \& Engn, Beijing 100084, Peoples R China.
   Tsing Hua Univ, Dept Mat Sci \& Engn, Beijing 100084, Peoples R China.}},
DOI = {{10.1016/j.cattod.2004.04.027}},
ISSN = {{0920-5861}},
EISSN = {{1873-4308}},
Keywords = {{perovskite; coprecipitation; nitrogen oxides; lean exhaust}},
Keywords-Plus = {{PEROVSKITE-TYPE CATALYSTS; NITRIC-OXIDE; SIMULTANEOUS REMOVAL; PLUS CO;
   OXYGEN; SR; DECOMPOSITION}},
Research-Areas = {{Chemistry; Engineering}},
Web-of-Science-Categories  = {{Chemistry, Applied; Chemistry, Physical; Engineering, Chemical}},
Author-Email = {{wuxiaodong@tsinghua.edu.cn}},
Cited-References = {{Belessi VC, 2000, CATAL TODAY, V59, P347, DOI 10.1016/S0920-5861(00)00300-X.
   Belessi VC, 2000, APPL CATAL B-ENVIRON, V28, P13, DOI 10.1016/S0926-3373(00)00159-4.
   Blasin-Aube V, 2003, APPL CATAL B-ENVIRON, V43, P175, DOI 10.1016/S0926-3373(02)00302-8.
   Borovskikh L, 2003, SOLID STATE SCI, V5, P409, DOI 10.1016/S1293-2558(03)00052-9.
   Buciuman FC, 2001, APPL CATAL B-ENVIRON, V35, P149, DOI 10.1016/S0926-3373(01)00249-1.
   Burch R, 2001, APPL CATAL A-GEN, V210, P63, DOI 10.1016/S0926-860X(00)00790-0.
   Ferri D, 1998, APPL CATAL B-ENVIRON, V16, P339, DOI 10.1016/S0926-3373(97)00090-8.
   Fino D, 2003, APPL CATAL B-ENVIRON, V43, P243, DOI 10.1016/S0926-3373(02)00311-9.
   Harada T, 1997, APPL SURF SCI, V121, P505, DOI 10.1016/S0169-4332(97)00354-1.
   Hodjati S, 2000, APPL CATAL B-ENVIRON, V26, P5, DOI 10.1016/S0926-3373(99)00143-5.
   Hong SS, 2000, CATAL TODAY, V63, P397, DOI 10.1016/S0920-5861(00)00484-3.
   Resini C, 2003, J CATAL, V214, P179, DOI 10.1016/S0021-9517(02)00153-7.
   Tanaka H, 2001, CURR OPIN SOLID ST M, V5, P381, DOI 10.1016/S1359-0286(01)00035-3.
   Tanaka H, 2003, APPL CATAL A-GEN, V244, P371, DOI 10.1016/S0926-860X(02)00609-9.
   Teraoka Y, 2001, APPL CATAL B-ENVIRON, V34, P73, DOI 10.1016/S0926-3373(01)00202-8.
   Tofan C, 2002, APPL CATAL B-ENVIRON, V36, P311, DOI 10.1016/S0926-3373(01)00312-5.
   Tofan C, 2002, APPL CATAL A-GEN, V226, P225, DOI 10.1016/S0926-860X(01)00908-5.}},
Number-of-Cited-References = {{17}},
Times-Cited = {{30}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{10}},
Journal-ISO = {{Catal. Today}},
Doc-Delivery-Number = {{848YQ}},
Unique-ID = {{ISI:000223504500005}},
DA = {{2020-08-06}},
}

@article{ ISI:000222574800005,
Author = {Giannini, A and Saravanan, R and Chang, P},
Title = {{The preconditioning role of Tropical Atlantic Variability in the
   development of the ENSO teleconnection: implications for the prediction
   of Nordeste rainfall}},
Journal = {{CLIMATE DYNAMICS}},
Year = {{2004}},
Volume = {{22}},
Number = {{8}},
Pages = {{839-855}},
Month = {{JUL}},
Abstract = {{A comparison of rainfall variability in the semi-arid Brazilian Nordeste
   in observations and in two sets of model simulations leads to the
   conclusion that the evolving interaction between Tropical Atlantic
   Variability (TAV) and the El Nino-Southern Oscillation (ENSO) phenomenon
   can explain two puzzling features of ENSO's impact on the Nordeste: (1)
   the event-to-event unpredictability of ENSO's impact; (2) the greater
   impact of cold rather than warm ENSO events during the past 50 years.
   The explanation is in the `preconditioning' role of Tropical Atlantic
   Variability. When, in seasons prior to the mature phase of ENSO, the
   tropical Atlantic happens to be evolving consistently with the
   development expected of the ENSO teleconnection, ENSO and TAV add up to
   force large anomalies in Nordeste rainfall. When it happens to be
   evolving in opposition to the canonical development of ENSO, then the
   net outcome is less obvious, but also less anomalous. The more frequent
   occurrence of tropical Atlantic conditions consistent with those that
   develop during a cold ENSO event, i.e. of a negative meridional sea
   surface temperature gradient, explains the weaker warm ENSO and stronger
   cold ENSO anomalies in Nordeste rainfall of the latter part of the
   twentieth century. Close monitoring of the evolution of the tropical
   Atlantic in seasons prior to the mature phase of ENSO should lead to an
   enhanced forecast potential.}},
Publisher = {{SPRINGER}},
Address = {{ONE NEW YORK PLAZA, SUITE 4600, NEW YORK, NY, UNITED STATES}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Giannini, A (Corresponding Author), Int Res Inst Climate Predict, POB 1000, Palisades, NY 10964 USA.
   Natl Ctr Atmospher Res, Boulder, CO 80307 USA.
   Texas A\&M Univ, Dept Oceanog, College Stn, TX 77843 USA.}},
DOI = {{10.1007/s00382-004-0420-2}},
ISSN = {{0930-7575}},
EISSN = {{1432-0894}},
Keywords-Plus = {{SEA-SURFACE TEMPERATURE; NORTHEAST BRAZIL; CLIMATE VARIABILITY;
   SOUTHERN-OSCILLATION; INTERDECADAL CHANGES; ATMOSPHERIC BRIDGE; SST
   ANOMALIES; OCEAN; PACIFIC; PRECIPITATION}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
Author-Email = {{alesall@iri.columbia.edu}},
ResearcherID-Numbers = {{Saravanan, Ramalingam/G-8879-2012
   Chang, Ping/A-1642-2013
   Giannini, Alessandra/H-4403-2013
   Giannini, Alessandra/F-7163-2016}},
ORCID-Numbers = {{Saravanan, Ramalingam/0000-0002-0005-6907
   Chang, Ping/0000-0002-9085-0759
   Giannini, Alessandra/0000-0001-5425-4995}},
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Number-of-Cited-References = {{55}},
Times-Cited = {{76}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{7}},
Journal-ISO = {{Clim. Dyn.}},
Doc-Delivery-Number = {{836RZ}},
Unique-ID = {{ISI:000222574800005}},
DA = {{2020-08-06}},
}

@article{ ISI:000223496900010,
Author = {Lenzen, M and Dey, C and Foran, B},
Title = {{Energy requirements of Sydney households}},
Journal = {{ECOLOGICAL ECONOMICS}},
Year = {{2004}},
Volume = {{49}},
Number = {{3}},
Pages = {{375-399}},
Month = {{JUL 1}},
Abstract = {{Supporting the lifestyles of the populations of modem cities requires
   vast quantities of natural resources and leads to environmental stresses
   such as air and water pollution. Research into the metabolism of cities
   therefore aims at understanding the physical flows into, within, and out
   of cities with a view to reducing the use of resources and the
   environmental impacts. One important physical indicator is energy use.
   Most studies on cities only consider direct or end-user energy
   consumption. Since the function of cities is to serve the lives of their
   residents, indirect energy use in cities, or energy embodied in the
   consumption of goods and services by its residents, can be regarded as
   being as important as direct energy use. However, physical models of
   cities are extremely complex and have difficulty in dealing with
   boundary issues, and hence the indirect resource requirements. In this
   paper we use input-output analysis and detailed household expenditure
   data to yield comprehensive energy use breakdowns for the 14 Statistical
   Subdivisions of Sydney. Multivariate regression and structural path
   analysis (SPA) are used to interpret the results. Clear correlations can
   be drawn between energy use and income, household size, age, and degree
   of urbanity. The structural path analysis is used to demonstrate how
   significant differences in lifestyles between inner and outer areas of
   Sydney leads to different energy use characteristics. This final
   consumption-based approach to analysing the energy requirements for
   households has important implications for measures aimed at reducing
   energy use, which tend to only consider direct energy use. (C) 2004
   Elsevier B.V. All rights reserved.}},
Publisher = {{ELSEVIER}},
Address = {{RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS}},
Type = {{Review}},
Language = {{English}},
Affiliation = {{Lenzen, M (Corresponding Author), Univ Sydney, Sch Phys, A28, Sydney, NSW 2006, Australia.
   Univ Sydney, Sch Phys, Sydney, NSW 2006, Australia.
   CSIRO, Sustainable Ecosyst, Resource Futures Program, Canberra, ACT 2601, Australia.}},
DOI = {{10.1016/j.ecolecon.2004.01.019}},
ISSN = {{0921-8009}},
EISSN = {{1873-6106}},
Keywords = {{household consumption; input-output analysis; embodied energy; spatial
   distribution; correlation; regression; city metabolism; urban
   sustainability}},
Keywords-Plus = {{INPUT-OUTPUT TECHNIQUES; ECOLOGICAL FOOTPRINT; ELECTRICITY CONSUMPTION;
   GREENHOUSE GASES; LAND-USE; CITIES; COST; SUSTAINABILITY; ENVIRONMENT;
   MANAGEMENT}},
Research-Areas = {{Environmental Sciences \& Ecology; Business \& Economics}},
Web-of-Science-Categories  = {{Ecology; Economics; Environmental Sciences; Environmental Studies}},
Author-Email = {{m.lenzen@physics.usyd.edu.au
   c.dey@physics.usyd.edu.au
   Barney.Foran@csiro.au}},
ResearcherID-Numbers = {{feng, tingting/A-9545-2012
   Lenzen, Manfred/D-3161-2013
   }},
ORCID-Numbers = {{Lenzen, Manfred/0000-0002-0828-5288}},
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