text:
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Number-of-Cited-References = {{51}},
Times-Cited = {{0}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{6}},
Doc-Delivery-Number = {{BT59X}},
Unique-ID = {{ISI:000173446300076}},
OA = {{Bronze}},
DA = {{2020-08-06}},
}

@article{ ISI:000170559000023,
Author = {Farkas, A and Rozsa, P},
Title = {{Data perturbations of matrices of pairwise comparisons}},
Journal = {{ANNALS OF OPERATIONS RESEARCH}},
Year = {{2001}},
Volume = {{101}},
Pages = {{401-425}},
Abstract = {{This paper deals with data perturbations of pairwise comparison matrices
   (PCM). Transitive and symmetrically reciprocal (SR) matrices are
   defined. Characteristic polynomials and spectral properties of certain
   SR perturbations of transitive matrices are presented. The principal
   eigenvector components of some of these PCMs are given in explicit form.
   Results are applied to PCMs occurring in various fields of interest,
   such as in the analytic hierarchy process (AHP) to the paired comparison
   matrix entries of which are positive numbers, in the dynamic
   input-output analysis to the matrix of economic growth elements of which
   might become both positive and negative and in vehicle system dynamics
   to the input spectral density matrix whose entries are complex numbers.}},
Publisher = {{SPRINGER}},
Address = {{VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Farkas, A (Corresponding Author), IMC Grad Sch Business, Dept Prod \& Operat Res, Zrinyi 14, H-1051 Budapest, Hungary.
   IMC Grad Sch Business, Dept Prod \& Operat Res, H-1051 Budapest, Hungary.
   Tech Univ Budapest, Dept Comp Sci, H-1521 Budapest, Hungary.}},
DOI = {{10.1023/A:1010986321720}},
ISSN = {{0254-5330}},
EISSN = {{1572-9338}},
Research-Areas = {{Operations Research \& Management Science}},
Web-of-Science-Categories  = {{Operations Research \& Management Science}},
Author-Email = {{farkas@imc.hu
   rozsa@math.bme.hu}},
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Number-of-Cited-References = {{21}},
Times-Cited = {{6}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{3}},
Journal-ISO = {{Ann. Oper. Res.}},
Doc-Delivery-Number = {{464XQ}},
Unique-ID = {{ISI:000170559000023}},
DA = {{2020-08-06}},
}

@article{ ISI:000208100700007,
Author = {Massacand, Alexia C. and Davies, Huw C.},
Title = {{Interannual Variability of European Winter Weather: The Potential
   Vorticity Insight}},
Journal = {{ATMOSPHERIC SCIENCE LETTERS}},
Year = {{2001}},
Volume = {{2}},
Number = {{1-4}},
Pages = {{52-60}},
Month = {{JAN}},
Abstract = {{Consideration of well-established teleconnection patterns account for
   only a moderate part of European winter variations. Here January
   interannual variability is examined from a potential vorticity
   perspective and this yields a reappraisal of the pattern structure and
   link to European winter weather. The influence of a novel hemispheric
   pattern in particular is detected. (C) 2001 Royal Meteorological Society}},
Publisher = {{WILEY-BLACKWELL}},
Address = {{COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Massacand, AC (Corresponding Author), ETH Honggerberg, Inst Atmospher Sci ETH, HPP, CH-8093 Zurich, Switzerland.
   Massacand, Alexia C.; Davies, Huw C., ETH, Inst Atmospher Sci, Zurich, Switzerland.}},
DOI = {{10.1006/asle.2001.0026}},
ISSN = {{1530-261X}},
Keywords = {{Interannual variations; teleconnections; European weather; potential
   vorticity}},
Research-Areas = {{Geochemistry \& Geophysics; Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Geochemistry \& Geophysics; Meteorology \& Atmospheric Sciences}},
Author-Email = {{massacand@atmos.umnw.ethz.ch}},
ResearcherID-Numbers = {{DAVIES, HUW C/A-6654-2008}},
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Number-of-Cited-References = {{21}},
Times-Cited = {{9}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{1}},
Journal-ISO = {{Atmos. Sci. Lett.}},
Doc-Delivery-Number = {{V19VU}},
Unique-ID = {{ISI:000208100700007}},
DA = {{2020-08-06}},
}

@article{ ISI:000208100700008,
Author = {Massacand, Alexia C. and Davies, Huw C.},
Title = {{Interannual variability of the extratropical northern hemisphere and the
   potential vorticity wave guide}},
Journal = {{ATMOSPHERIC SCIENCE LETTERS}},
Year = {{2001}},
Volume = {{2}},
Number = {{1-4}},
Pages = {{61-71}},
Month = {{JAN}},
Abstract = {{Interrannual flow variations in the extratropics are reappraised from a
   potential vorticity (PV) perspective. A statistical study of the
   patterns of PV variability on a tropopause-transecting isentropic
   surface provides a compact description of, and dynamical insight into,
   the Pacific-North American teleconnection and the North Atlantic
   Oscillation. (C) 2001 Royal Meteorological Society}},
Publisher = {{WILEY-BLACKWELL}},
Address = {{COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Massacand, AC (Corresponding Author), ETH Honggerberg, HPP, Inst Atmospher Sci, ETH, CH-8093 Zurich, Switzerland.
   Massacand, Alexia C., ETH Honggerberg, HPP, Inst Atmospher Sci, ETH, CH-8093 Zurich, Switzerland.}},
DOI = {{10.1006/asle.2001.0027}},
ISSN = {{1530-261X}},
Keywords = {{Interannual variability; PNA; NAO; potential vorticity}},
Research-Areas = {{Geochemistry \& Geophysics; Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Geochemistry \& Geophysics; Meteorology \& Atmospheric Sciences}},
Author-Email = {{massacand@atmos.umnw.ethz.ch}},
ResearcherID-Numbers = {{DAVIES, HUW C/A-6654-2008}},
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Number-of-Cited-References = {{31}},
Times-Cited = {{7}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{0}},
Journal-ISO = {{Atmos. Sci. Lett.}},
Doc-Delivery-Number = {{V19VU}},
Unique-ID = {{ISI:000208100700008}},
DA = {{2020-08-06}},
}

@article{ ISI:000166226800004,
Author = {Collins, M and Tett, SFB and Cooper, C},
Title = {{The internal climate variability of HadCM3, a version of the Hadley
   Centre coupled model without flux adjustments}},
Journal = {{CLIMATE DYNAMICS}},
Year = {{2001}},
Volume = {{17}},
Number = {{1}},
Pages = {{61-81}},
Month = {{JAN}},
Abstract = {{We examine the internal climate variability of a 1000 year long
   integration of the third version of the Hadley Centre coupled model
   (HadCM3). The model requires no flux adjustment, needs no spin up
   procedure prior to coupling and has a stable climate in the global mean.
   The principal aims are (I) to validate the internal climate variability
   against observed climate variability, (2) to examine the model for any
   periodic modes of variability, (3) to use the model estimate of internal
   climate variability to asses the probability of occurrence of observed
   trends in climate variables, and (4) to compare HadCM3 with the previous
   version of the Hadley Centre model, HadCM2. The magnitude and frequency
   characteristics of the variability of the global mean surface
   temperature of HadCM3 on annual to decadal time scales is in good
   agreement with the observations. Observed upward trends in temperature
   over the last 20 years and longer are inconsistent with the internal
   variability of the model. The simulated spatial pattern of surface
   temperature variability is qualitatively similar to that observed,
   although there is an overestimation of the land temperature variability
   and regional errors in ocean temperature variability. The model
   simulates an El Nino Southern Oscillation with an irregular 3-4 year
   cycle, and with a teleconnection pattern which is much more like the
   observations than was found in HadCM2. The interdecadal variability of
   the model ocean in the tropical Pacific, North Pacific and North
   Atlantic is broadly similar to that in the real world with none of the
   simulated patterns having any periodic behaviour. HadCM3 simulates an
   Arctic Oscillation/North Atlantic Oscillation (NAO) in Northern
   Hemisphere winter which has a spatial pattern consistent with the
   observations in the Atlantic region, but has too much teleconnection
   with the North Pacific. The recent observed upward trend in the NAO
   index is inconsistent with the model internal variability. The
   variability of the simulated zonal mean atmospheric temperature shows
   some marked differences to the observed zonal mean temperature
   variability, although the comparison is confounded by the sparse
   observational network and its possible contamination by a climate change
   signal.}},
Publisher = {{SPRINGER-VERLAG}},
Address = {{175 FIFTH AVE, NEW YORK, NY 10010 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Collins, M (Corresponding Author), Meteorol Off, Hadley Ctr Climate Predict \& Res, London Rd, Bracknell RG12 2SZ, Berks, England.
   Meteorol Off, Hadley Ctr Climate Predict \& Res, Bracknell RG12 2SZ, Berks, England.}},
DOI = {{10.1007/s003820000094}},
ISSN = {{0930-7575}},
Keywords-Plus = {{NORTH-ATLANTIC OSCILLATION; OCEAN CIRCULATION MODELS; OFFICE UNIFIED
   MODEL; TEMPERATURE; SURFACE; TRENDS; IMPACT; GCM; PACIFIC; SIMULATION}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
ResearcherID-Numbers = {{Collins, Matthew/F-8473-2011
   Tett, Simon F. B./B-1504-2013}},
ORCID-Numbers = {{Collins, Matthew/0000-0003-3785-6008
   Tett, Simon F. B./0000-0001-7526-560X}},
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Number-of-Cited-References = {{60}},
Times-Cited = {{291}},
Usage-Count-Last-180-days = {{2}},
Usage-Count-Since-2013 = {{30}},
Journal-ISO = {{Clim. Dyn.}},
Doc-Delivery-Number = {{389EZ}},
Unique-ID = {{ISI:000166226800004}},
DA = {{2020-08-06}},
}

@article{ ISI:000167527300002,
Author = {Hu, ZZ and Bengtsson, L and Roeckner, E and Christoph, M and Bacher, A
   and Oberhuber, JM},
Title = {{Impact of global warming on the interannual and interdecadal climate
   modes in a coupled GCM}},
Journal = {{CLIMATE DYNAMICS}},
Year = {{2001}},
Volume = {{17}},
Number = {{5-6}},
Pages = {{361-374}},
Abstract = {{In this study, we investigated the impact of global warming on the
   variabilities of large-scale interannual and interdecadal climate modes
   and teleconnection patterns with two long-term integrations of the
   coupled general circulation model of ECHAM4/OPYC3 at the
   Max-Planck-Institute for Meteorology, Hamburg. One is the control (CTRL)
   run with fixed present-day; concentrations of greenhouse gases. The
   other experiment is a simulation of transient greenhouse warming, named
   GHG run. In the GHG run the averaged geopotential height at 500 hPa is
   increased significantly, and a negative phase of the Pacific/North
   American (PNA) teleconnection-like distribution pattern is intensified.
   The standard deviation over the tropics thigh latitudes) is enhanced
   (reduced) on the interdecadal time scales and reduced (enhanced) on the
   interannual time scales in the GHG run. Except for an interdecadal mode
   related to the Southern Oscillation (SO) in the GHG run, the spatial
   variation patterns are similar for different (interannual +
   interdecadal, interannual, and interdecadal) time scales in the GHG and
   CTRL runs. Spatial distributions of the teleconnection patterns on the
   interannual and interdecadal time scales in the GHG run are also similar
   to those in the CTRL run. But some teleconnection patterns show linear
   trends and changes of variances and frequencies in the GHG run. Apart
   from the positive linear trend of the SO, the interdecadal modulation to
   the El Nino/SO cycle is enhanced during the GHG 2040 similar to 2099.
   This is the result of an enhancement of the Walker circulation during
   that period. La Nino events intensify and El Nino events relatively
   weaken during the GHG 2070 similar to 2090. It is interesting to note
   that with increasing greenhouse gas concentrations the relation between
   the SO and the PNA pattern is reversed significantly from a negative to
   a positive correlation on the interdecadal time scales and weakened on
   the interannual time scales. This suggests that the increase of the
   greenhouse gas concentrations will trigger the nonstationary correlation
   between the SO and the PNA pattern both on the interdecadal and
   interannual time scales.}},
Publisher = {{SPRINGER-VERLAG}},
Address = {{175 FIFTH AVE, NEW YORK, NY 10010 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Hu, ZZ (Corresponding Author), Ctr Ocean Land Atmosphere Studies, Beltsville, MD 20705 USA.
   Ctr Ocean Land Atmosphere Studies, Beltsville, MD 20705 USA.
   Max Planck Inst Meteorol, D-20146 Hamburg, Germany.
   Deutsch Klimarechenzentrum GmbH, D-20146 Hamburg, Germany.}},
DOI = {{10.1007/PL00013737}},
ISSN = {{0930-7575}},
Keywords-Plus = {{GENERAL-CIRCULATION MODEL; OCEAN-ATMOSPHERE MODEL; SOUTHERN OSCILLATION;
   NORTHERN-HEMISPHERE; TROPICAL PACIFIC; HEIGHT FIELD; VARIABILITY; CO2;
   ENSO; SIMULATION}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
ResearcherID-Numbers = {{Hu, Zeng-Zhen/B-4373-2011}},
ORCID-Numbers = {{Hu, Zeng-Zhen/0000-0002-8485-3400}},
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Number-of-Cited-References = {{54}},
Times-Cited = {{14}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{5}},
Journal-ISO = {{Clim. Dyn.}},
Doc-Delivery-Number = {{411YM}},
Unique-ID = {{ISI:000167527300002}},
DA = {{2020-08-06}},
}

@inproceedings{ ISI:000173272300033,
Author = {Frias, MD and Rodriguez-Puebla, C},
Editor = {{India, MB and Bonillo, DL}},
Title = {{Time-frequency variability of spring precipitation associated with
   teleconnection indices over the Iberian peninsula.}},
Booktitle = {{DETECTING AND MODELLING REGIONAL CLIMATE CHANGE}},
Year = {{2001}},
Pages = {{389-396}},
Note = {{International Scientific Meeting on the Detection and Modelling of
   Recent Climate Change and its Effects on a Regional Scale, TARRAGONA,
   SPAIN, MAY, 2000}},
Organization = {{Rovira \& Virgili Univ, Climate Change Res Grp; Autonomous Govt
   Catalonian, Environm Dept Catalonian Meterol Serv}},
Abstract = {{The economic consequences of periods of rain and drought are one of the
   primary motivations for performing this study which is focused on
   obtaining stable periodic modes of precipitation and identifying the
   underlying physical processes involved. Singular Spectral Analysis (SSA)
   combined with the Maximum Entropy Method (MEM) were applied to some of
   the longest available precipitation time series located in different
   climatic regions over the Iberian Peninsula. The spectral analysis of
   samples, by moving the series starting time, was performed. Once the
   stable peaks were identified, a cross-spectral analysis between the
   precipitation time series and the North Hemisphere teleconnection
   indices was computed. The links in the spectral domain can be of great
   interest to determine dependence in the short or long term and
   therefore, to improve statistical prediction models. The North
   Hemisphere Annular mode and the Southern Oscillation Index were found to
   covary with spring precipitation observations at the interannual time
   scale.}},
Publisher = {{SPRINGER-VERLAG BERLIN}},
Address = {{HEIDELBERGER PLATZ 3, D-14197 BERLIN, GERMANY}},
Type = {{Proceedings Paper}},
Language = {{English}},
Affiliation = {{Frias, MD (Corresponding Author), Univ Salamanca, Dept Atmospher Phys, E-37008 Salamanca, Spain.
   Univ Salamanca, Dept Atmospher Phys, E-37008 Salamanca, Spain.}},
ISBN = {{3-540-42239-0}},
Keywords-Plus = {{NORTH-ATLANTIC OSCILLATION; SINGULAR-SPECTRUM ANALYSIS; NINO SOUTHERN
   OSCILLATION; INTRASEASONAL OSCILLATIONS; EXTRATROPICAL CIRCULATION;
   GLOBAL ATMOSPHERE; SEASONAL RAINFALL; ANNULAR MODES; PATTERNS;
   TEMPERATURE}},
Research-Areas = {{Physical Geography; Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Geography, Physical; Meteorology \& Atmospheric Sciences}},
ResearcherID-Numbers = {{Rodriguez-Puebla, Concepcion/C-1414-2011
   Frias, Maria Dolores MD/F-4874-2012}},
ORCID-Numbers = {{Rodriguez-Puebla, Concepcion/0000-0003-0018-6805
   }},
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Number-of-Cited-References = {{33}},
Times-Cited = {{0}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{1}},
Doc-Delivery-Number = {{BT53J}},
Unique-ID = {{ISI:000173272300033}},
DA = {{2020-08-06}},
}

@inproceedings{ ISI:000173272300037,
Author = {Orgaz, MDM and Caramelo, L},
Editor = {{India, MB and Bonillo, DL}},
Title = {{Spatial and temporal variability of the surface air temperature over the
   Duero Basin (Iberian peninsula)}},
Booktitle = {{DETECTING AND MODELLING REGIONAL CLIMATE CHANGE}},
Year = {{2001}},
Pages = {{429-438}},
Note = {{International Scientific Meeting on the Detection and Modelling of
   Recent Climate Change and its Effects on a Regional Scale, TARRAGONA,
   SPAIN, MAY, 2000}},
Organization = {{Rovira \& Virgili Univ, Climate Change Res Grp; Autonomous Govt
   Catalonian, Environm Dept Catalonian Meterol Serv}},
Abstract = {{In this study we have investigated the spatial and temporal variability
   of 48 year annual temperature series for 40 meteorological stations
   distributed in the Duero Basin.
   Empirical orthogonal functions were used to identify spatial variation
   patterns in the temperature anomalies. This method allowed the
   identification of four regional temperature regimes. The four leading
   EOFs accounts for 81 \% of total variance.
   The structure of the temporal variations was obtained by applying a
   spectral method (F.F.T.) to the corresponding principal components
   (PCs).
   The correlation between PCs and some teleconnection indices (North
   Atlantic Oscillation (NAO) and Southern Oscillation Index (SOI)) were
   also investigated.}},
Publisher = {{SPRINGER-VERLAG BERLIN}},
Address = {{HEIDELBERGER PLATZ 3, D-14197 BERLIN, GERMANY}},
Type = {{Proceedings Paper}},
Language = {{English}},
Affiliation = {{Orgaz, MDM (Corresponding Author), Univ Aveiro, Dept Fis, P-3800 Aveiro, Portugal.
   Univ Aveiro, Dept Fis, P-3800 Aveiro, Portugal.}},
ISBN = {{3-540-42239-0}},
Keywords-Plus = {{SOUTH-EASTERN USA; TELECONNECTION PATTERNS; CIRCULATION; ANOMALIES;
   WINTER}},
Research-Areas = {{Physical Geography; Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Geography, Physical; Meteorology \& Atmospheric Sciences}},
ResearcherID-Numbers = {{Caramelo, Liliana/K-1729-2013}},
ORCID-Numbers = {{Caramelo, Liliana/0000-0001-5740-3167}},
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Number-of-Cited-References = {{17}},
Times-Cited = {{0}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{1}},
Doc-Delivery-Number = {{BT53J}},
Unique-ID = {{ISI:000173272300037}},
DA = {{2020-08-06}},
}

@inproceedings{ ISI:000175456800033,
Author = {Kobayashi, K and Chonan, M and Matsuzaki, H and Shirakawa, N},
Editor = {{Li, G}},
Title = {{The life cycle assessment and cost-benefit analysis for nature friendly
   river works}},
Booktitle = {{DEVELOPMENT, PLANNING AND MANAGEMENT OF SURFACE AND GROUND WATER
   RESOURCES, THEME A, PROCEEDINGS}},
Year = {{2001}},
Pages = {{215-220}},
Note = {{29th Annual Congress of the
   International-Association-of-Hydraulic-Engineering-and-Research (IAHR),
   BEIJING INT CONVENT CTR, BEIJING, PEOPLES R CHINA, SEP 16-21, 2001}},
Organization = {{Int Assoc Hydraul Engn \& Res; Minist Water Resources; Natl Nat Sci Fdn
   China; United Nat Educ, Sci \& Cultural Org; Hai River Conservancy
   Commiss; Huai River Conservancy Commiss; Songhua River \& Liao River
   Conservancy Commiss; Xialangdi Multipurpose Project Corp; China Yangtze
   Three Gorges Project Dev Corp; China Inst Water Resources \& Hydropower
   Res}},
Abstract = {{In recent years ecological aspects in streams have been a center of
   public attention. Nature friendly river works, which have been done by
   mainly nature material since 1981, are well known to have an effect of
   reducing CO2. However almost nature friendly river works are more
   expensive than conventional river works. Namely nature friendly river
   works have destiny trade-off between environment and money. The
   necessity of the project evaluation of a public works rises. Especially,
   the value of the environment is remarkable. Then we should evaluate
   clearly the value of river environment in point of money.
   We proposed the LCA method. The effect of the reduction of CO2 is
   evaluating analyzed. The LCA evaluation of the Tama River Basin was
   concretely done by the input-output analysis of inter-industry
   relationships. The input-output analysis was pursued from money the
   effect to all industries which the reduction of CO2 brought respect.
   We proposed the cost-benefit analysis to put the benefit of the river
   environment together in the effect of the stock of river works in the
   past investigation. The System for Integrated Environmental Economic
   Accounting was made based on the I/O table which was in existence. The
   effect of flow was calculated by applying this to actual river works for
   environmental improvement.}},
Publisher = {{TSINGHUA UNIVERSITY PRESS}},
Address = {{TSINGHUA UNIVERSITY HAIDIANQU, BEIJING 100084, PEOPLES R CHINA}},
Type = {{Proceedings Paper}},
Language = {{English}},
Affiliation = {{Kobayashi, K (Corresponding Author), CTI Engn Co Ltd, Hokuriku Branch, 2-4-10,Higashi Oodori, Niigata 9500087, Japan.
   CTI Engn Co Ltd, Hokuriku Branch, Niigata 9500087, Japan.}},
ISBN = {{7-302-04676-X}},
Keywords = {{CO2; river planning; SEEA; I/O analysis; value for river environment;
   environmental policy}},
Research-Areas = {{Engineering; Water Resources}},
Web-of-Science-Categories  = {{Engineering, Civil; Water Resources}},
Cited-References = {{SHIMATANI Y, 1998, REDUCTION CO2 NATURE, V40, P56.
   SHIRAKAWA N, 2000, S RIV ENG, V6, P243.
   UCHIYAMA Y, 1993, ENERG ECON, P27.}},
Number-of-Cited-References = {{3}},
Times-Cited = {{0}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{5}},
Doc-Delivery-Number = {{BU24A}},
Unique-ID = {{ISI:000175456800033}},
DA = {{2020-08-06}},
}

@article{ ISI:000170467700006,
Author = {Moffatt, I and Hanley, N},
Title = {{Modelling sustainable development: systems dynamic and input-ouput
   approaches}},
Journal = {{ENVIRONMENTAL MODELLING \& SOFTWARE}},
Year = {{2001}},
Volume = {{16}},
Number = {{6, SI}},
Pages = {{545-557}},
Abstract = {{This paper discusses alternative approaches to modelling
   economy-environment systems from the perspective of sustainable
   development. We distinguish between systems' dynamic methods and
   economic approaches, including input-output (I/O) models. We then
   discuss the structure of two models constructed for Scotland. Firstly, a
   hierarchical, dynamic model is used to look at long-term trends in
   population, resource use and pollution. Secondly, an environmentally
   extended I/O model is used to estimate the effects of economic policy
   and structural change on pollution levels and output. We conclude with
   some comments on the possible future developments in modelling
   sustainable development. (C) 2001 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 = {{Moffatt, I (Corresponding Author), Univ Stirling, Dept Environm Sci, Stirling FK9 4LA, Scotland.
   Univ Stirling, Dept Environm Sci, Stirling FK9 4LA, Scotland.
   Univ Glasgow, Dept Econ, Glasgow G12 8QQ, Lanark, Scotland.}},
DOI = {{10.1016/S1364-8152(01)00024-X}},
ISSN = {{1364-8152}},
Keywords = {{sustainable development; dynamic systems; hierarchical modelling;
   input-output analysis}},
Keywords-Plus = {{ENVIRONMENTAL-POLICY; OUTPUT-ANALYSIS; QUALITY; COST}},
Research-Areas = {{Computer Science; Engineering; Environmental Sciences \& Ecology}},
Web-of-Science-Categories  = {{Computer Science, Interdisciplinary Applications; Engineering,
   Environmental; Environmental Sciences}},
Cited-References = {{ALLEN P, 1981, ENVIRON PLANN A, V21, P167.
   BOYD R, 1991, J POLICY MODEL, V13, P115, DOI 10.1016/0161-8938(91)90005-J.
   Brekke K.A., 1997, EC GROWTH ENV MEASUR.
   CASLER S, 1984, RESOUR ENERG, V6, P187, DOI 10.1016/0165-0572(84)90016-1.
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   CONRAD K, 1993, J POLICY MODEL, V15, P521, DOI 10.1016/0161-8938(93)90004-A.
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   JORGENSON DW, 1990, RAND J ECON, V21, P314, DOI 10.2307/2555426.
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   Moffatt I., 1992, International Journal of Environmental Studies, V41, P225, DOI 10.1080/00207239208710761.
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   Moffatt I, 2001, MEASURING MODELLING.
   MOFFATT I, 1989, P 3 EUR C ED, P220.
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   Muller F, 1979, ENERGY ENV INTERREGI.
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   PEARCE F, 1998, NEW SCI 112, V2142.
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   PEARSON PJG, 1989, ENVIRON PLANN A, V21, P1329, DOI 10.1068/a211329.
   PRIGOGINE I, 1982, ORDER OUT OF CHAOS.
   PROOPS JLR, 1992, REDUCINT CO2 EMISSIO.
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   Schafer D., 1989, ECON SYST RES, V1, P203.
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   VOS J, 1983, ENV PLANNING INFORMA.
   World Commission on Environment and Development (WCED), 1987, OUR COMM FUT.}},
Number-of-Cited-References = {{51}},
Times-Cited = {{27}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{7}},
Journal-ISO = {{Environ. Modell. Softw.}},
Doc-Delivery-Number = {{463GA}},
Unique-ID = {{ISI:000170467700006}},
DA = {{2020-08-06}},
}

@inproceedings{ ISI:000223815200022,
Author = {Dukic, B and Novak, N},
Editor = {{UgarcicHardi, Z}},
Title = {{Information supported input/output analysis of production capacities of
   bread grains in eastern Slavonia}},
Booktitle = {{FLOUR - BREAD ` 01}},
Year = {{2001}},
Pages = {{180-192}},
Note = {{International Congress on Flour - Bread/3rd Croatian Congress of Cereal
   Technologists, Opatija, CROATIA, NOV 14-17, 2001}},
Organization = {{Minist Znanosti Tehnol Republ Hrvatske; TIM ZIP; Diamant Ges m b H \& Co
   KG; Belisce d d Tvorn Papira Ambalaze; Trgo Pak d d}},
Abstract = {{Privately and state-owned capacities for cultivating bread grains in
   eastern Slavonia are an important resource of that part of Croatia. A
   complex task necessary for the achievement of main strategic goals in
   agriculture development is the design and utilization of an adequate
   input/output model for the analysis of the production, business,
   warehousing and service systems, supported by information and
   communication technologies. Computer support of such a model has for
   some time been an imperative of successful agricultural production.
   The model would ensure efficient management of agricultural production
   within family farms, but also at higher coordinating and administrative
   levels. To further develop manufacturing capacities, it is necessary to
   optimally utilize available arable land by a direct production analysis
   of all soil types and their capacity in bread grain production.
   The design, introduction and maintenance of a computerized input/output
   model of bread grain production in eastern Slavonia, based on a
   well-designed data basis on all the attributes of agricultural
   production, can help in achieving those goals.
   Natural indices on types and quantities of cultivated bread grains,
   available crops and classes of arable land, utilized plant protection
   and other agro-technical measures for increasing the quality and
   quantity of production are a precondition for permanent improvement of
   crop production.
   The paper describes the technological and organizational approach to the
   modeling of input/output analysis by using available information on the
   fanning incentives in the region. The paper discusses measurable and
   immeasurable effects of modem information technology, the support it can
   provide to different users, and some realization procedures.
   An integral part of a computerized model of input/output analysis of
   bread grain production are data bases on land-registry, crops and land
   classes according to ownership, as well as natural indices in bread
   grain production with usual technologies. The paper discusses control
   procedures in creating the sowing}},
Publisher = {{UNIV JOSIP JURAJ STROOSSMAYER OSIJEK}},
Address = {{FACULTY FOOD TECHNOLOGY, DEPT FLOUR PRODUCTION PROCESSING TECHNOLOGY,
   OSIJEK, HRVATSKA 31000, CROATIA}},
Type = {{Proceedings Paper}},
Language = {{English}},
Affiliation = {{Dukic, B (Corresponding Author), Sveuciliste JJ Strosssmayera Osijeku, Ekonomski Fak Osijeku, Gajev Trg 7, Osijek, Croatia.
   Sveuciliste JJ Strosssmayera Osijeku, Ekonomski Fak Osijeku, Osijek, Croatia.}},
ISBN = {{953-97478-9-9}},
Keywords = {{input/output analysis; information system; arable land; bread grains;
   standards in processing of bread grains}},
Research-Areas = {{Food Science \& Technology}},
Web-of-Science-Categories  = {{Food Science \& Technology}},
Cited-References = {{BABIC M, 1990, OSNOVE INPUT OUTPUT.
   COURTNEY F, 1988, DATABASE SYSTEMS MAN.
   GAGNON G, 1999, MREZA, V10, P74.
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   MARTIC LJ, 1982, MATEMATICKE METODE E.
   PANIAN Z, 2000, ELEKTRONICKO TRGOVAN.
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   Tkalac S., 1993, RELACIJSKI MODEL POD.
   Varga M., 1994, BAZE PODATAKA KONCEP.}},
Number-of-Cited-References = {{10}},
Times-Cited = {{1}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{1}},
Doc-Delivery-Number = {{BAV68}},
Unique-ID = {{ISI:000223815200022}},
DA = {{2020-08-06}},
}

@inproceedings{ ISI:000177297200395,
Author = {Chasmer, LE and LeDrew, EF},
Book-Group-Author = {{IEEE
   IEEE}},
Title = {{Weekly interactions between sea ice concentrations and the North
   Atlantic oscillation in the Odden sea ice peninsula, Greenland Sea}},
Booktitle = {{IGARSS 2001: SCANNING THE PRESENT AND RESOLVING THE FUTURE, VOLS 1-7,
   PROCEEDINGS}},
Series = {{IEEE International Symposium on Geoscience and Remote Sensing IGARSS}},
Year = {{2001}},
Pages = {{1249-1251}},
Note = {{IEEE International Geoscience and Remote Sensing Symposium, UNIV NEW S
   WALES, SYDNEY, AUSTRALIA, JUL 09-13, 2001}},
Organization = {{IEEE; IEEE, Geosci \& Remote Sensing Soc; NASA; US Dept Commerce, Natl
   Ocean \& Atmosphere Adm; CSA ASC; Off Naval Res; RSPAA; URSI}},
Abstract = {{In this study, we use principal components analysis and a discrete
   wavelet decomposition to examine changing patterns of sea ice within the
   Odden ice peninsula, Greenland Sea. Daily passive microwave satellite
   imagery collected by tile National Snow and Ice Data Center (NSIDC),
   Colorado have been subset to include ice concentrations within a 22 x 40
   pixel region located between 72 and 74 degrees North Latitude. The Odden
   is a curious feature because it rapidly changes form in the course of
   days to weeks, whereby shape is highly dependent upon areas of ice melt
   and growth. In {[}1] we found numerous connections between the Odden and
   the North Atlantic Oscillation (NAO), a Northern Hemisphere atmospheric
   teleconnection pattern. The most prominent similarities occurred
   seasonally, as is to be expected from the seasonal properties of the NAO
   (for example, its usually positive mode during winter, corresponding to
   colder temperatures). However by examining smaller spatial and temporal
   changes within the Odden, we find both correspondence and anomalies
   between the NAO and changing sea ice concentrations. During some
   weeks/months we find a strong positive correlation between the Odden and
   the NAO, whereby the NAO leads sea ice development by a few days.
   However, during other dines, we find that the NAO signal may be dampened
   by other meteorological/oceanographic events, and therefore, the signals
   are opposite or un-related. These results may be good indicators of
   ice/atmosphere interactions that occur in relation with the NAO.}},
Publisher = {{IEEE}},
Address = {{345 E 47TH ST, NEW YORK, NY 10017 USA}},
Type = {{Proceedings Paper}},
Language = {{English}},
Affiliation = {{Chasmer, LE (Corresponding Author), Univ Waterloo, Waterloo Lab Earth Observat, Dept Geog, Waterloo, ON N2L 3G1, Canada.
   Univ Waterloo, Waterloo Lab Earth Observat, Dept Geog, Waterloo, ON N2L 3G1, Canada.}},
ISSN = {{2153-6996}},
ISBN = {{0-7803-7031-7}},
Keywords-Plus = {{FIELD}},
Research-Areas = {{Engineering; Geology; Remote Sensing}},
Web-of-Science-Categories  = {{Engineering, Electrical \& Electronic; Geosciences, Multidisciplinary;
   Remote Sensing}},
Author-Email = {{lechasme@fes.uwaterloo.ca}},
Cited-References = {{CHASMER L, 2001, THESIS U WATERLOO WA.
   CHASMER LE, 2001, P AM MET SOC 6 C MET.
   Martin T, 1999, DEEP-SEA RES PT II, V46, P1063, DOI 10.1016/S0967-0645(99)00016-8.
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   WALLACE JM, 1981, MON WEATHER REV, V109, P784, DOI 10.1175/1520-0493(1981)109<0784:TITGHF>2.0.CO;2.}},
Number-of-Cited-References = {{9}},
Times-Cited = {{1}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{0}},
Doc-Delivery-Number = {{BU88J}},
Unique-ID = {{ISI:000177297200395}},
DA = {{2020-08-06}},
}

@article{ ISI:000169040200001,
Author = {Hess, JC and Scott, CA and Hufford, GL and Fleming, MD},
Title = {{El Nino and its impact on fire weather conditions in Alaska}},
Journal = {{INTERNATIONAL JOURNAL OF WILDLAND FIRE}},
Year = {{2001}},
Volume = {{10}},
Number = {{1}},
Pages = {{1-13}},
Abstract = {{Examining the relationship of El Nino to weather patterns in Alaska
   shows wide climate variances that depend on the teleconnection between
   the tropics and the northern latitudes. However, the weather patterns
   exhibited in Alaska during and just after moderate to strong El Nino
   episodes are generally consistent: above normal temperature and
   precipitation along the Alaskan coast, and above normal temperature and
   below normal precipitation in the interior, especially through the
   winter. The warm, dry conditions in the Alaskan interior increase summer
   wildfire potential. Statistics on the area burned since 1940 show that
   15 out of 17 of the biggest fire years occurred during a moderate to
   strong El Nino episode. These 15 years account for nearly 63\% of the
   total area burned over the last 58 years. Evidence points to increased
   dry thunderstorms and associated lightning activity during an El Nino
   episode; the percentage of total area burned by lightning caused fires
   during five episodes increased from a normal of less than 40\% to a high
   of about 96\%.}},
Publisher = {{INT ASSOC WILDLAND FIRE}},
Address = {{PO BOX 2156, CLANCY, MT 59634-2156 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Hess, JC (Corresponding Author), Natl Weather Serv, Alaska Reg, 222 W 7th Ave, Anchorage, AK 99513 USA.
   Anchorage Weather Serv, Forecast Off, Anchorage, AK 99502 USA.}},
DOI = {{10.1071/WF01007}},
ISSN = {{1049-8001}},
Keywords = {{El Nino; ENSO; Alaska; wildfires; weather patterns; burned area}},
Keywords-Plus = {{SOUTHERN OSCILLATION; ATMOSPHERIC CIRCULATION; UNITED-STATES; ANOMALIES}},
Research-Areas = {{Forestry}},
Web-of-Science-Categories  = {{Forestry}},
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   WALLACE JM, 1981, MON WEA REV, V109, P1150.}},
Number-of-Cited-References = {{18}},
Times-Cited = {{46}},
Usage-Count-Last-180-days = {{2}},
Usage-Count-Since-2013 = {{13}},
Journal-ISO = {{Int. J. Wildland Fire}},
Doc-Delivery-Number = {{438EF}},
Unique-ID = {{ISI:000169040200001}},
DA = {{2020-08-06}},
}

@article{ ISI:000166857800007,
Author = {Yin, JH and Battisti, DS},
Title = {{The importance of tropical sea surface temperature patterns in
   simulations of last glacial maximum climate}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2001}},
Volume = {{14}},
Number = {{4}},
Pages = {{565-581}},
Abstract = {{Prescribed SST experiments are performed using the National Center for
   Atmospheric Research's Community Climate Model version 3 general
   circulation model to isolate the contribution of the tropical SSTs
   reconstructed by the Climate, Long-range Investigation, Mapping and
   Prediction study (CLIMAP) to the modeled global atmospheric circulation
   anomalies at the Last Glacial Maximum (LGM). The changes in tropical SST
   patterns cause changes in tropical convection that force large (>300 m
   in 500-mb geopotential height) changes in Northern Hemisphere wintertime
   circulation. These midlatitude circulation changes occur despite the
   small (1 degreesC) change in the mean tropical SST between the present
   and the CLIMAP reconstruction. In fact, the midlatitude circulation
   changes due to the difference in the tropical SST pattern between the
   present and the CLIMAP reconstruction are greater than the circulation
   changes due to a uniform tropical SST cooling of 3 degreesC or those due
   to the presence of the LGM ice sheets. The circulation anomalies due to
   the change in tropical SST patterns result in a wintertime warming
   (cooling) of 8 degreesC (8 degreesC) over the Laurentide (Fennoscandian)
   ice sheet and a decrease (increase) in annual mass balance of over 1000
   mm yr (-1) (800 mm yr(-1)) along the southern margin of the ice sheet.
   These results demonstrate that detailed knowledge of tropical SST
   patterns is needed in order to produce reliable simulations of LGM
   climate. In the appendix, it is shown that the lion's share of the
   midlatitude circulation changes are due to SST gradients in the northern
   Tropics, and that the physics involved in the teleconnection between
   tropical SST forcing and midlatitude circulation changes is rich and
   highly nonlinear.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Yin, JH (Corresponding Author), Univ Washington, Joint Inst Study Atmosphere \& Oceans, Dept Atmospher Sci, Box 354235, Seattle, WA 98195 USA.
   Univ Washington, Joint Inst Study Atmosphere \& Oceans, Dept Atmospher Sci, Seattle, WA 98195 USA.}},
DOI = {{10.1175/1520-0442(2001)014<0565:TIOTSS>2.0.CO;2}},
ISSN = {{0894-8755}},
Keywords-Plus = {{GENERAL-CIRCULATION MODEL; WAVE-PROPAGATION; ICE SHEETS; OCEAN;
   ATMOSPHERE; VARIABILITY; CYCLE; ENSO}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
ResearcherID-Numbers = {{Battisti, David S/A-3340-2013}},
ORCID-Numbers = {{Battisti, David S/0000-0003-4871-1293}},
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Number-of-Cited-References = {{33}},
Times-Cited = {{76}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{11}},
Journal-ISO = {{J. Clim.}},
Doc-Delivery-Number = {{400DW}},
Unique-ID = {{ISI:000166857800007}},
DA = {{2020-08-06}},
}

@article{ ISI:000167674000002,
Author = {Cash, BA and Lee, S},
Title = {{Observed nonmodal growth of the Pacific-North American teleconnection
   pattern}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2001}},
Volume = {{14}},
Number = {{6}},
Pages = {{1017-1028}},
Abstract = {{A linear-stochastic model is applied to the 10-day low-pass
   streamfunction field at 300, 500, and 850 mb for 40 winter seasons of
   Northern Hemisphere NCEP-NCAR reanalysis data. The linear operator is
   derived from the observed multilevel covariances, allowing for
   statistical representation of nonlinear processes. While all empirical
   normal modes of the system are decaying, increase in the streamfunction
   variance is possible through nonmodal growth. When the evolution of the
   streamfunction field following the optimal perturbation is predicted,
   the Pacific-North American teleconnection pattern (PNA) is found to be
   the most probable state of the atmosphere. Sixty-eight percent (70\%) of
   positive (negative) PNA events are found to follow high projections onto
   the leading optimal, suggesting the PNA arises through constructive
   interference between the decaying modes and may be treated as a linear
   response to Gaussian white noise stochastic forcing. Implications for
   PNA timescale and onset mechanisms are also discussed.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Cash, BA (Corresponding Author), Geophys Fluid Dynam Lab, POB 308,Forrestal Campus, Princeton, NJ 08542 USA.
   Penn State Univ, Dept Meteorol, University Pk, PA 16802 USA.}},
DOI = {{10.1175/1520-0442(2001)014<1017:ONGOTP>2.0.CO;2}},
ISSN = {{0894-8755}},
Keywords-Plus = {{SURFACE TEMPERATURE ANOMALIES; FREQUENCY; INSTABILITY; OSCILLATION;
   FLOW; GCM}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
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Number-of-Cited-References = {{24}},
Times-Cited = {{31}},
Usage-Count-Last-180-days = {{0}},
Usage-Count-Since-2013 = {{4}},
Journal-ISO = {{J. Clim.}},
Doc-Delivery-Number = {{414NY}},
Unique-ID = {{ISI:000167674000002}},
DA = {{2020-08-06}},
}

@article{ ISI:000167674000018,
Author = {Hoerling, MP and Kumar, A and Xu, TY},
Title = {{Robustness of the nonlinear climate response to ENSO's extreme phases}},
Journal = {{JOURNAL OF CLIMATE}},
Year = {{2001}},
Volume = {{14}},
Number = {{6}},
Pages = {{1277-1293}},
Abstract = {{Analysis of a suite of atmospheric GCM experiments for 1950-94 shows
   that both the tropical and the extratropical wintertime climate respond
   nonlinearly with respect to opposite phases of ENSO. Such behavior is
   found to be reproducible among four different GCMs studied and confirms
   that several observed asymmetries in wintertime anomalies with respect
   to ENSO phases are symptomatic of nonlinearity rather than sampling
   error.
   Nonlinearity in the tropical Pacific rainfall response is related to an
   SST threshold for convection that leads to saturation at modestly cold
   SST forcing but a linear increase for warmer SST forcing. A spatial
   shift in the rainfall response is also a feature of the various GCMs'
   nonlinear behavior, that is, accentuated by the large zonal gradient of
   climatological SSTs across the equatorial Pacific and the fact that
   convection responds to the total rather than the anomalous SST.
   Regarding upper-tropospheric teleconnection responses over the
   Pacific-North American region, nonlinearity exists in both the strength
   of the midlatitude response and its spatial phase. The four GCMs are
   found to be unanimous in having a 500-mb height response whose amplitude
   is roughly double for extreme warm tropical Pacific SSTs as compared
   with extreme cold SST forcing. The longitudinal phase of the GCMs'
   teleconnections is also shifted eastward during warm events as compared
   with cold events, though this displacement is smaller than that
   observed.
   Further analysis of model simulations reveals that nonlinearity in
   climate responses emerges mainly for stronger ENSO events, and a
   predominantly linear response is found for weaker tropical Pacific SST
   forcing. In particular, climate simulations using both realistic and
   idealized SSTs indicate that tropical Pacific SST anomalies greater than
   one standard deviation of the interannual variation are required for
   initiating an appreciable nonlinear climate response.}},
Publisher = {{AMER METEOROLOGICAL SOC}},
Address = {{45 BEACON ST, BOSTON, MA 02108-3693 USA}},
Type = {{Article}},
Language = {{English}},
Affiliation = {{Hoerling, MP (Corresponding Author), NOAA, CIRES, Climate Diagnost Ctr, R-E-CD,325 Broadway, Boulder, CO 80303 USA.
   NOAA, CIRES, Climate Diagnost Ctr, Boulder, CO 80303 USA.
   NOAA, NCEP, Washington, DC USA.}},
DOI = {{10.1175/1520-0442(2001)014<1277:ROTNCR>2.0.CO;2}},
ISSN = {{0894-8755}},
Keywords-Plus = {{SEA-SURFACE TEMPERATURE; EL-NINO EVENT; ANOMALIES; TELECONNECTIONS;
   VARIABILITY; SIMULATIONS; HEMISPHERE; RAINFALL; STATES; MODEL}},
Research-Areas = {{Meteorology \& Atmospheric Sciences}},
Web-of-Science-Categories  = {{Meteorology \& Atmospheric Sciences}},
ResearcherID-Numbers = {{, AK/B-6517-2008}},
Cited-References = {{ARKIN PA, 1987, MON WEATHER REV, V115, P51, DOI 10.1175/1520-0493(1987)115<0051:TRBLSC>2.0.CO;2.
   BROCCOLI AJ, 1992, J CLIMATE, V5, P1181, DOI 10.1175/152

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