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Books on the topic 'Wet climate'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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1

Wet and dry. Riverstream Publishing, 2013.

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2

Wet and dry places. Amicus, 2012.

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3

Singh, Nityanand. Climatic and hydroclimatic features of wet and dry spells and their extremes across India. Indian Institute of Tropical Meteorology, 2009.

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4

Cheung, Chan Chik. Synoptic patterns associated with wet and dry northerly cold surges of the northeast monsoon. Royal Observatory, 1997.

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5

Eddy, Richard L. Variability of wet and dry periods in the Upper Colorado River Basin and the possible effects of climate change and sensitivity of probable maximum precipitation estimates to climate change. U.S. Dept. of the Interior, Bureau of Reclamation, Denver Office, 1996.

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6

How the West was warmed: Responding to climate change in the Rockies. Fulcrum, 2009.

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7

Conover, Beth. How the West was warmed: Responding to climate change in the Rockies. Fulcrum, 2009.

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8

Changjiang yuan qu qi hou bian hua ji qi sheng tai shui wen ying xiang. Qi xiang chu ban she, 2008.

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9

Hayward, Derek F. Climatology of West Africa. Hutchinson Education, 1987.

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10

Hayward, Derek F. The climatology of West Africa. Hutchinson, 1987.

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11

Basu, Jyotish Prakash. Climate Change Vulnerability and Communities in Agro-climatic Regions of West Bengal, India. Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-50468-7.

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12

Lesher, David C. The climate of Canaan Valley, West Virginia. D.C. Lesher, 2003.

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13

Keen, Richard A. Skywatch west: The complete weather guide. Fulcrum, 2004.

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14

Jiqiang, Fu, ed. Da qian yi: Nuan hua ru he ying xiang ni wo de wei lai. Tian xia za zhi gu fen you xian gong si, 2009.

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15

Sandford, Robert W. Water, weather and the Mountain West. Rocky Mountain Books, 2007.

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16

Sandford, Robert W. Water, weather and the mountain West. Rocky Mountain Books, 2007.

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17

West African agriculture and climate change: A comprehensive analysis. International Food Policy Research Institute, 2013.

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18

Ybema, Klaas. Wat een weer!: Kroniek van het weer in Friesland 1901-2006. Friese Pers Boekerij, 2007.

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19

Kumar, M. V. K. Siva. Agroclimatology of West Africa: Burkina Faso. International Crops Research Institute for the Semi-Arid Tropics, 1987.

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20

Bidlake, W. R. Evapotranspiration from areas of native vegetation in West-Central Florida. U.S. G.P.O., 1996.

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21

Yaro, Joseph A., and Jan Hesselberg, eds. Adaptation to Climate Change and Variability in Rural West Africa. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-31499-0.

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22

Shaoping, Chen, ed. Chang Jiang shang you zhi hong bao yu tian wen tian qi ou he yu bao fang fa yan jiu ji ying yong. Qi xiang chu ban she, 2001.

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23

Xilinhaote guo jia qi hou guan xiang tai lun wen ji: 2006.01-2010.12. Qi xiang chu ban she, 2011.

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24

Sivakumar, Mannava V. K., Rattan Lal, Ramasamy Selvaraju, and Ibrahim Hamdan, eds. Climate Change and Food Security in West Asia and North Africa. Springer Netherlands, 2013. http://dx.doi.org/10.1007/978-94-007-6751-5.

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25

Weidick, Anker. Neoglacial and historical glacier changes around Kangersuneq Fjord in southern West Greenland. Geological Survey of Denmark and Greenland, Danish Ministry of Climate and Energy, 2012.

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26

Zollinger, Marc. Die Schwörers: Wie die Welt zum Kinderzimmer wurde. Wörterseh, 2009.

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27

Xinjiang qi xiang xue hui cheng li 40 zhou nian lun wen ji. Qi xiang chu ban she, 2005.

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28

Weaver, Bobby D. Hotter 'n pecos and other west Texas lies. Texas Tech University Press, 2010.

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29

Hotter 'n pecos and other west Texas lies. Texas Tech University Press, 2010.

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30

A Wet Look At Climate Change. Bookboon.com, 2013.

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31

Ingram, Scott E. Climate. Edited by Barbara Mills and Severin Fowles. Oxford University Press, 2017. http://dx.doi.org/10.1093/oxfordhb/9780199978427.013.40.

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This chapter serves as an introduction to and reference for climate–human behavior studies in the Southwest. These studies investigate potential climatic impacts on social change and historical trajectories. To build foundational understanding, a representative climate–human behavior model is presented and evaluated, commonly used paleoclimatic data are detailed, and methods for identifying climate extremes (e.g., droughts, wet periods) in these data are described. Some extreme climate events and the challenge of identifying their influence (if any) on social change are noted. A familiarity wi

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32

A Wet Look At Climate Change Hurricanes to House Mites. Bookboon.com, 2013.

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33

A Wet Look At Climate Change Hurricanes to House Mites. Bookboon, 2013.

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34

A Wet Look At Climate Change Hurricanes to House Mites. Bookboon.com, 2013.

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35

B, Elsner James, and United States. National Aeronautics and Space Administration., eds. Large-scale circulation departures related to wet episodes in northeast Brazil. Atmospheric Sciences Division, Dept. of Geological/Geophysical Sciences, University of Wisconsin, 1985.

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36

B, Elsner James, and United States. National Aeronautics and Space Administration., eds. Large-scale circulation departures related to wet episodes in northeast Brazil. Atmospheric Sciences Division, Dept. of Geological/Geophysical Sciences, University of Wisconsin, 1985.

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37

Mackey, Brendan, David Lindenmayer, Malcolm Gill, Michael McCarthy, and Janette Lindesay, eds. Wildlife, Fire and Future Climate. CSIRO Publishing, 2002. http://dx.doi.org/10.1071/9780643090040.

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The conservation of Earth's forest ecosystems is one of the great environmental challenges facing humanity in the 21st century. All of Earth's ecosystems now face the spectre of the accelerated greenhouse effect and rates of change in climatic regimes that have hitherto been unknown. In addition, multiple use forestry – where forests are managed to provide for both a supply of wood and the conservation of biodiversity – can change the floristic composition and vegetation structure of forests with significant implications for wildlife habitat. Wildlife, fire and future climate: a forest e

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38

Heckman, Charles W. Rice Field Ecology in Northeastern Thailand: The Effect Of Wet And Dry Seasons On A Cultivated Aquatic Ecosystem. Springer, 2013.

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39

Behera, Swadhin, and Toshio Yamagata. Climate Dynamics of ENSO Modoki Phenomena. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.612.

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The El Niño Modoki/La Niña Modoki (ENSO Modoki) is a newly acknowledged face of ocean-atmosphere coupled variability in the tropical Pacific Ocean. The oceanic and atmospheric conditions associated with the El Niño Modoki are different from that of canonical El Niño, which is extensively studied for its dynamics and worldwide impacts. A typical El Niño event is marked by a warm anomaly of sea surface temperature (SST) in the equatorial eastern Pacific. Because of the associated changes in the surface winds and the weakening of coastal upwelling, the coasts of South America suffer from widespre

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40

Goswami, B. N., and Soumi Chakravorty. Dynamics of the Indian Summer Monsoon Climate. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.613.

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Lifeline for about one-sixth of the world’s population in the subcontinent, the Indian summer monsoon (ISM) is an integral part of the annual cycle of the winds (reversal of winds with seasons), coupled with a strong annual cycle of precipitation (wet summer and dry winter). For over a century, high socioeconomic impacts of ISM rainfall (ISMR) in the region have driven scientists to attempt to predict the year-to-year variations of ISM rainfall. A remarkably stable phenomenon, making its appearance every year without fail, the ISM climate exhibits a rather small year-to-year variation (the sta

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41

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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42

How the West was warmed: Responding to climate change in the Rockies. Fulcrum Pub., 2010.

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43

Beth, Conover, ed. How the West was warmed: Responding to climate change in the Rockies. Fulcrum Pub., 2009.

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44

Chubarova, Natalia, Yekaterina Zhdanova, Yelizaveta Androsova, et al. THE AEROSOL URBAN POLLUTION AND ITS EFFECTS ON WEATHER, REGIONAL CLIMATE AND GEOCHEMICAL PROCESSES. LLC MAKS Press, 2020. http://dx.doi.org/10.29003/m1475.978-5-317-06464-8.

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The monograph is devoted to the study of atmospheric aerosol and its dynamics in the urban environment of Moscow megacity. Based on the AeroRadCity 2018-2019 complex experiment, composed of measurement campaign and numerical experiments using the COSMO-ART chemical transport model, a number of new results were obtained, which contributed to a deeper understanding of the gas-aerosol composition of the urban atmosphere, wet aerosol deposition with accounting of geochemical processes and aerosol radiative effects. Aerosol pollution in the Moscow region and its dynamics in the 21st century were es

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45

Esler, Karen J., Anna L. Jacobsen, and R. Brandon Pratt. Characteristics of Mediterranean-Type Ecosystems. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198739135.003.0002.

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Modern mediterranean-type ecosystems (MTEs) are shaped by key ecosystem drivers that affect their function. The most important of these drivers are climate, topography, soils, and fire. There are important geographical, climatic, and fire histories that are crucial to understanding these systems. Mediterranean-type climate (MTC) is defined as a cool wet winter (winter-wet) and a warm dry summer, which is a unique pattern of seasonality and one that is rare globally. All of the MTC regions have nutrient-poor soils, particularly as related to nitrogen (N), and some also have extensive phosphorus

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46

(Editor), A. J. Dietz, R. Ruben (Editor), and A. Verhagen (Editor), eds. The Impact of Climate Change on Drylands: With a focus on West Africa (Environment & Policy). Springer, 2004.

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47

Zalasiewicz, Jan, and Mark Williams. The Goldilocks Planet. Oxford University Press, 2012. http://dx.doi.org/10.1093/oso/9780199593576.001.0001.

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Climate change is a major topic of concern today and will be so for the foreseeable future, as predicted changes in global temperatures, rainfall, and sea level continue to take place. But as Jan Zalasiewicz and Mark Williams reveal in The Goldilocks Planet, the climatic changes we are experiencing today hardly compare to the changes the Earth has seen over the last 4.5 billion years. Indeed, the vast history that the authors relate here is dramatic and often abrupt--with massive changes in global and regional climate, from bitterly cold to sweltering hot, from arid to humid. They introduce us

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48

Canada. Dept. of Agriculture., ed. Canadian north-west: Climate and productions : a misrepresentation exposed. 5th ed. Dept. of Agriculture, 1986.

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49

(India), National Climate Centre, and India. Dept. of Publication., eds. Climate of West Bengal. Controller of Publications, 2008.

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50

(India), National Climate Centre, and India. Dept. of Publication., eds. Climate of West Bengal. Controller of Publications, 2008.

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