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Books on the topic 'Global circulation models'

Author: Grafiati

Published: 4 June 2021

Last updated: 4 February 2022

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1

Justus, C. G. Mars Global Reference Atmospheric Model 2001 Version (Mars-GRAM 2001): Users guide. National Aeronautics and Space Administration, George C. Marshall Space Flight Center, 2001.

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2

V, Ramesh K. Time-mean oceanic response and interannual variability in a global ocean GCM simulation. Indian Institute of Tropical Meteorology, 2003.

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3

Justus, C. G. The NASA/MSFC global reference atmospheric model--1990 version (GRAM-90). School of Earth and Atmospheric Sciences, Georgia Institue of Technology, 1990.

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4

Rapp, Richard H. The development of a degree 360 expansion of the dynamic ocean topography of the POCM4̲B global circulation model. National Aeronautics and Space Administration, Goddard Space Flight Center, 1998.

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5

Moore, Berrien. Global analysis, interpretation and modelling: An earth systems modelling program : final report, NASA grant # NAGW 4706. National Aeronautics and Space Administration, 1997.

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6

Workshop on Cloud Microphysics Parameterizations in Global Atmospheric Circulation Models (1995 Kananaskis, Alta.). Workshop on Cloud Microphysics Parameterizations in Global Atmospheric Circulation Models: Kananaskis, Alberta, Canada, 23-25 May 1995. Joint Planning Staff for WCRP c/o World Meteorological Organization, 1995.

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7

Vincent, Dayton G. Observational and modeling studies of heat, moisture, precipitation and global-scale circulation patterns: Final technical report, July 20, 1990 - January 19, 1994. National Aeronautics and Space Administration, 1994.

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8

Indo-US Seminar on Parameterization of Sub-grid Scale Processes in Dynamical Models of Medium Range Prediction and Global Climate (1990 Pune, India). Physical processes in atmospheric models: Collection of papers presented at the Indo-US Seminar on Parameterization of Sub-grid Scale Processes in Dynamical Models of Medium Range Prediction and Global Climate, IITM, Pune, India, 6-10 August 1990. Wiley, 1992.

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9

Office, General Accounting. Global warming: Limitations of general circulation models and costs of modeling efforts : report to the Ranking Minority Member, Committee on Commerce, House of Representatives. The Office, 1995.

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10

Los, Sietse Oene. Linkages between global vegetation and climate: An analysis based on NOAA advanced very high resolution radiometer data : contract NAS-31752. National Aeronautics and Space Administration, Goddard Space Flight Center, 1998.

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11

Justus, C. G. The NASA/MSFC Global Reference Atmospheric Model--1999 version (GRAM-99). National Aeronautics and Space Administration, Marshall Space Flight Center, 1999.

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12

Justus, C. G. The NASA/MSFC Global Reference Atmospheric Model--1999 version (GRAM-99). National Aeronautics and Space Administration, Marshall Space Flight Center, 1999.

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13

Justus, C. G. The NASA/MSFC Global Reference Atmospheric Model--1999 version (GRAM-99). National Aeronautics and Space Administration, Marshall Space Flight Center, 1999.

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14

Brix, Holger. North Atlantic deep water and Antarctic bottom water: Their interaction and influence on modes of the global ocean circulation = Die wechselseitige Beeinflussung von Nordatlantischem Tiefenwasser und antarktischem Bodenwasser und ihre Rolle für globale Moden der ozeanischen Zirkulation. Alfred-Wegener-Institut für Polar- und Meeresforschung, 2001.

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15

Service, Canadian Forest, and Rocky Mountain Research Station (Fort Collins, Colo.), eds. High resolution interpolation of climate scenarios for the conterminous USA and Alaska derived from general circulation model simulations. U.S. Dept. of Agriculture, Forest Service, Rocky Mountain Research Station, 2011.

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16

Grotch, Stanley L. An intercomparison of general circulation model predictions of regional climate change: Presented at the International Conference on "Modelling of Global Climate Change and Variability," Hamburg, Federal Republic of Germany, September 1989. Available from National Technical Information Service, 1990.

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17

C, Sud Y., Kim J. H, and Goddard Space Flight Center, eds. Intercomparison of hydrologic processes in global climate models. National Aeronautics and Space Administration, Goddard Space Flight Center, 1995.

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18

1939-, Justus C. G., and George C. Marshall Space Flight Center., eds. The NASA/MSFC global reference atmospheric model--1995 version (GRAM-95). National Aeronautics and Space Administration, Marshall Space Flight Center, 1995.

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19

General circulation model output for forest climate change research and applications. U.S. Dept. of Agriculture, Forest Service, Southeastern Forest Experiment Station, 1993.

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20

General circulation model output for forest climate change research and applications. U.S. Dept. of Agriculture, Forest Service, Southeastern Forest Experiment Station, 1993.

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21

Global analysis, interpretation and modelling: An earth systems modelling program : final report, NASA grant # NAGW 4706. National Aeronautics and Space Administration, 1997.

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22

How dry is the tropical free troposphere?: Implications for global warming theory. National Aeronautics and Space Administration, 1997.

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23

D, Braswell William, and United States. National Aeronautics and Space Administration., eds. How dry is the tropical free troposphere?: Implications for global warming theory. National Aeronautics and Space Administration, 1997.

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24

(Editor), Soroosh Sorooshian, Hoshin V. Gupta (Editor), and John C. Rodda (Editor), eds. Land Surface Processes in Hydrology: Trials and Tribulations of Modeling and Measuring (NATO ASI Series / Global Environmental Change). Springer, 1997.

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25

C, Bridger Alison F., Haberle Robert M, and United States. National Aeronautics and Space Administration., eds. Mars Global Surveyor: Aerobraking and observations support using a Mars global circulation model : a NASA Ames Research Center Joint Research Interchange, final report : university consortium agreement NCC2-5148; project duration, 25 July 1995-24 October 1997. National Aeronautics and Space Administration, 1997.

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26

C, Bridger Alison F., Haberle Robert M, and United States. National Aeronautics and Space Administration., eds. Mars Global Surveyor: Aerobraking and observations support using a Mars global circulation model : a NASA Ames Research Center Joint Research Interchange, final report : university consortium agreement NCC2-5148; project duration, 25 July 1995-24 October 1997. National Aeronautics and Space Administration, 1997.

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27

O, Manning James, and United States. National Aeronautics and Space Administration., eds. A study of carbon monoxide distribution determinations for a global transport model. National Aeronautics and Space Administration, 1987.

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28

Center, Goddard Space Flight, ed. A coupled ocean general circulation, biogeochemical, and radiative model of the global oceans: Seasonal distributions of ocean chlorophyll and nutrients. National Aeronautics and Space Administration, Goddard Space Flight Center, 2000.

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29

United States. National Aeronautics and Space Administration., ed. A study of carbon monoxide distribution determinations for a global transport model: Final report. Dept. of Chemical Engineering, University of Kentucky, 1988.

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30

Lurcock, Pontus, and Fabio Florindo. Antarctic Climate History and Global Climate Changes. Oxford University Press, 2017. http://dx.doi.org/10.1093/oxfordhb/9780190676889.013.18.

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Antarctic climate changes have been reconstructed from ice and sediment cores and numerical models (which also predict future changes). Major ice sheets first appeared 34 million years ago (Ma) and fluctuated throughout the Oligocene, with an overall cooling trend. Ice volume more than doubled at the Oligocene-Miocene boundary. Fluctuating Miocene temperatures peaked at 17–14 Ma, followed by dramatic cooling. Cooling continued through the Pliocene and Pleistocene, with another major glacial expansion at 3–2 Ma. Several interacting drivers control Antarctic climate. On timescales of 10,000–100,

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31

Lurcock, Pontus, and Fabio Florindo. Antarctic Climate History and Global Climate Changes. Oxford University Press, 2017. http://dx.doi.org/10.1093/oxfordhb/9780190699420.013.18.

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Antarctic climate changes have been reconstructed from ice and sediment cores and numerical models (which also predict future changes). Major ice sheets first appeared 34 million years ago (Ma) and fluctuated throughout the Oligocene, with an overall cooling trend. Ice volume more than doubled at the Oligocene-Miocene boundary. Fluctuating Miocene temperatures peaked at 17–14 Ma, followed by dramatic cooling. Cooling continued through the Pliocene and Pleistocene, with another major glacial expansion at 3–2 Ma. Several interacting drivers control Antarctic climate. On timescales of 10,000–100,

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32

Tibaldi, Stefano, and Franco Molteni. Atmospheric Blocking in Observation and Models. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.611.

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The atmospheric circulation in the mid-latitudes of both hemispheres is usually dominated by westerly winds and by planetary-scale and shorter-scale synoptic waves, moving mostly from west to east. A remarkable and frequent exception to this “usual” behavior is atmospheric blocking. Blocking occurs when the usual zonal flow is hindered by the establishment of a large-amplitude, quasi-stationary, high-pressure meridional circulation structure which “blocks” the flow of the westerlies and the progression of the atmospheric waves and disturbances embedded in them. Such blocking structures can hav

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33

United States. General Accounting Office, ed. Global warming: Limitations of general circulation models : statement of Peter F. Guerrero, Director, Environmental Protection Issues, Resources, Community, and Economic Development Division, before the Subcommittee on Energy and Environment, Committee on Science, House of Representatives. The Office, 1995.

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34

Thomas, Chyba, and United States. National Aeronautics and Space Administration., eds. Interpretation of lidar and satellite data sets using a global photochemical model: Progress report--July 31, 1996; NASA grant #NCC-1-214. National Aeronautics and Space Administration, 1996.

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35

1949-, Noda A., and Kokuritsu Kankyō Kenkyūjo. Chikyū Kankyō Kenkyū Sentā., eds. A new meteorological research institute coupled GCM (MRI-CGCM2): Transient response to greenhouse gas and aerosol scenarios. Center for Global Environmental Research, National Institute for Environmental Studies, Environment Agency of Japan, 2001.

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36

The Global Circulation of African Fashion (Dress, Body, Culture). Berg Publishers, 2002.

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37

Rabine, Leslie W. The Global Circulation of African Fashion (Dress, Body, Culture). Berg Publishers, 2002.

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38

Dunlop, Storm. 2. The circulation of the atmosphere. Oxford University Press, 2017. http://dx.doi.org/10.1093/actrade/9780199571314.003.0002.

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‘The circulation of the atmosphere’ outlines the general model of the movement of air around the Earth. There are three circulation cells either side of the equator: the Hadley cell (nearest to the equator) and the polar cell, driven by specific temperature and pressure gradients, and the Ferrel cell between them. It describes global pressure patterns and the Coriolis effect, which results in south-westerly trade winds in the northern hemisphere and north-westerly trade winds in the southern. Also described are the Intertropical Convergence Zone, the polar easterlies, the westerlies, and how a

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39

Busuioc, Aristita, and Alexandru Dumitrescu. Empirical-Statistical Downscaling: Nonlinear Statistical Downscaling. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.770.

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This is an advance summary of a forthcoming article in the Oxford Research Encyclopedia of Climate Science. Please check back later for the full article.The concept of statistical downscaling or empirical-statistical downscaling became a distinct and important scientific approach in climate science in recent decades, when the climate change issue and assessment of climate change impact on various social and natural systems have become international challenges. Global climate models are the best tools for estimating future climate conditions. Even if improvements can be made in state-of-the art

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40

Aram, B., and B. Yun-Casalilla. Global Goods and the Spanish Empire, 1492-1824: Circulation, Resistance and Diversity. Palgrave Macmillan, 2014.

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41

Aram, B., and B. Yun-Casalilla. Global Goods and the Spanish Empire, 1492-1824: Circulation, Resistance and Diversity. Palgrave Macmillan, 2014.

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42

Gao, Yanhong, and Deliang Chen. Modeling of Regional Climate over the Tibetan Plateau. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.591.

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The modeling of climate over the Tibetan Plateau (TP) started with the introduction of Global Climate Models (GCMs) in the 1950s. Since then, GCMs have been developed to simulate atmospheric dynamics and eventually the climate system. As the highest and widest international plateau, the strong orographic forcing caused by the TP and its impact on general circulation rather than regional climate was initially the focus. Later, with growing awareness of the incapability of GCMs to depict regional or local-scale atmospheric processes over the heterogeneous ground, coupled with the importance of t

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43

Vásquez, Manuel A., and David Garbin. Globalization. Edited by Michael Stausberg and Steven Engler. Oxford University Press, 2017. http://dx.doi.org/10.1093/oxfordhb/9780198729570.013.46.

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This chapter explores the key factors involved in the interaction between religion and globalization. It highlights the roles played by transnational networks, fields, and regimes, as well as migrant and religious diasporas, mass culture, and electronic media in the global circulation and appropriation of religious practices, beliefs, symbols, artifacts, and identities. Using the examples of religious networks associated with Islam, Hinduism, and Christianities, the chapter also argues that while the economic dimensions of religion in a context of globalization are central, the dynamics of glo

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44

Christensen, Ole Bøssing, and Erik Kjellström. Projections for Temperature, Precipitation, Wind, and Snow in the Baltic Sea Region until 2100. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.695.

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The ecosystems and the societies of the Baltic Sea region are quite sensitive to fluctuations in climate, and therefore it is expected that anthropogenic climate change will affect the region considerably. With numerical climate models, a large amount of projections of meteorological variables affected by anthropogenic climate change have been performed in the Baltic Sea region for periods reaching the end of this century.Existing global and regional climate model studies suggest that:• The future Baltic climate will get warmer, mostly so in winter. Changes increase with time or increasing emi

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45

The Role Of The Ocean In Global Cycling Of Persistent Organic Contaminants Refinement And Application Of A Global Multicompartment Chemistrytransport Model. Springer, 2010.

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46

(Editor), Wei-Chyung Wang, and I. S. A. Isaksen (Editor), eds. Atmospheric Ozone As a Climate Gas: General Circulation Model Simulations (Nato a S I Series Series I, Global Environmental Change). Springer-Verlag Telos, 1995.

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47

Freed, Joanne Lipson. Haunting Encounters. Cornell University Press, 2018. http://dx.doi.org/10.7591/cornell/9781501713767.001.0001.

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Beginning with the basic conviction that acts of cross-cultural reading have ethical consequences, Haunting Encounters traces the narrative strategies through which certain works fiction forge connections with their readers—in particular, their white, Western readers—across boundaries of difference. Through the formal and aesthetic negotiations they carry out, which both draw readers in and set limits on their imaginative engagements, these works respond in concrete ways to the asymmetries of their circulation and consumption in our contemporary global age. By bringing the tools and methods of

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48

Wang, Bin. Intraseasonal Modulation of the Indian Summer Monsoon. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.616.

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The strongest Indian summer monsoon (ISM) on the planet features prolonged clustered spells of wet and dry conditions often lasting for two to three weeks, known as active and break monsoons. The active and break monsoons are attributed to a quasi-periodic intraseasonal oscillation (ISO), which is an extremely important form of the ISM variability bridging weather and climate variation. The ISO over India is part of the ISO in global tropics. The latter is one of the most important meteorological phenomena discovered during the 20th century (Madden & Julian, 1971, 1972). The extreme dry an

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49

Barradas Jorge, Nuno. ReFocus: The Films of Pedro Costa. Edinburgh University Press, 2020. http://dx.doi.org/10.3366/edinburgh/9781474444538.001.0001.

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This is the first English-language study of internationally acclaimed Portuguese filmmaker Pedro Costa, examining the cultural, production and exhibition contexts of his feature films, shorts and video installations. It situates Costa’s filmmaking within the contexts of Portuguese, European and global art film, looking into his working practices alongside the impact of digital video, forms of collaborative authorship, and the intricate dialogue between modes of production and aesthetics. Considering the exhibition, circulation and reception of Costa’s creative output in settings such as film f

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50

Gano, Geneva M. The Little Art Colony and US Modernism. Edinburgh University Press, 2020. http://dx.doi.org/10.3366/edinburgh/9781474439756.001.0001.

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U.S. Modernism at Continent’s End: Carmel, Provincetown, Taos historicizes and theorizes the significance of the early twentieth-century little arts colony as a uniquely modern social formation within a global network of modernist activity and production. Emphasizing communities rather than single artists, and modernist activity instead of products, this study considers modernism as social, aesthetic, and political processes that developed differentially in response to local and global pressures. In addition to offering a historical overview of the emergence of three critical sites of modernis

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