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Volumn 316, Issue 5828, 2007, Pages 1181-1184

Model projections of an imminent transition to a more arid climate in southwestern North America

Author keywords

[No Author keywords available]

Indexed keywords

ANTHROPOGENIC EFFECT; ARID REGION; ARIDITY; CLIMATE CHANGE; CLIMATE FORCING; CLIMATE MODELING; REGIONAL DEVELOPMENT; RESOURCE ALLOCATION; WATER RESOURCE;

EID: 34249947530     PISSN: 00368075     EISSN: 10959203     Source Type: Journal    
DOI: 10.1126/science.1139601     Document Type: Article
Times cited : (1821)

References (16)
  • 3
    • 34249942658 scopus 로고    scopus 로고
    • Details of the models analyzed can be found at www-pcmdi.llnl.gov/ipcc/ model_documentation/ipcc_model_documentation.php, and the data can be found at https://esg.llnl.gov:8443/index.jsp.
    • Details of the models analyzed can be found at www-pcmdi.llnl.gov/ipcc/ model_documentation/ipcc_model_documentation.php, and the data can be found at https://esg.llnl.gov:8443/index.jsp.
  • 4
    • 0003564167 scopus 로고    scopus 로고
    • N. Nakicenovic, R. Swart, Eds, Cambridge Univ. Press, New York
    • N. Nakicenovic, R. Swart, Eds., Special Report on Emissions Scenarios (Cambridge Univ. Press, New York, 2000).
    • (2000) Special Report on Emissions Scenarios
  • 7
    • 34249933345 scopus 로고    scopus 로고
    • The model P - E is not fully accounted for by the computed moisture flow convergence that is calculated by taking the sum of the components of the mean flow and transient eddies (the imbalance is 0.022 mm/day). Calculations were performed with data collected daily on the model grid using closely matching numerics, but errors could be introduced by not using a time resolution of several hours and by neglecting moisture diffusion (potentially large over mountains), which was not archived. The data are available at http:/kage.ldeo.columbia.edu/SOURCES/.LDEO/.ClimateGroup/.GFDL.
    • The model P - E is not fully accounted for by the computed moisture flow convergence that is calculated by taking the sum of the components of the mean flow and transient eddies (the imbalance is 0.022 mm/day). Calculations were performed with data collected daily on the model grid using closely matching numerics, but errors could be introduced by not using a time resolution of several hours and by neglecting moisture diffusion (potentially large over mountains), which was not archived. The data are available at http:/kage.ldeo.columbia.edu/SOURCES/.LDEO/.ClimateGroup/.GFDL.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.