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1

Project, Dryland Adaptive Research, ed. Crop production workbook for arid and semi-arid lands. Natural Resources Institute, 1995.

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2

Baldy, Charles. Agrométéorologie et développement des régions arides et semi-arides. Institut national de la recherche agronomique, 1986.

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3

Henderson-Sellers, A., and A. J. Pitman, eds. Vegetation and climate interactions in semi-arid regions. Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-011-3264-0.

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4

Midgley, Stephanie. Adaptation to climate change in semi-arid environments: Experience and lessons from Mozambique. Food and Agriculture Organization of the United Nations, 2012.

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5

International Workshop on Climate Change in Arid and Semi-Arid Region of Asia (6th 2004 Ulaanbaatar, Mongolia). The sixth international workshop proceeding on climate change in arid and semi-arid regions of Asia: August 25-26, 2004, Ulaanbaatar, Mongolia. Institute of Meteorology and Hydrology, 2004.

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6

Souza Filho, Francisco de Assis., Moura Antônio Divino, Banco do Nordeste (Brazil), Fundação Cearense de Meteorologia e Recursos Hídricos., and International Research Institute for Climate Prediction., eds. Memórias do Seminário Natureza e Sociedade nos Semi-Áridos. Banco do Nordeste do Brasil, 2006.

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7

Wani, S. P., and K. V. Raju, eds. Community and Climate Resilience in the Semi-Arid Tropics. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-29918-7.

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8

Pandey, Rajendra Prasad. Drought characterization in arid and semi arid climatic regions of India. National Institute of Hydrology, 2000.

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9

Johansson, Erik. Watertightness of heavy flat roofs in semi-arid climates. 2nd ed. Lund University, Lund Centre for Habitat Studies, 1992.

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10

Conferência Internacional sobre Impactos de Variações Climáticas e Desenvolvimento Sustentável em Regiões Semi-Aridas (1992 Fortaleza, Brazil). Desenvolvimento e meio ambiente no semi-árido: Discursos e exposições especiais. Poder Legislativo, Senado Federal, Centro Gráfico, 1992.

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11

Sircoulon, Jacques. Impact possible des changements climatiques a venir sur les ressources en eau des regions arides et semi-arides: Comportement des cours d'eau tropicaux, des rivières et des lacs en zone sahélienne. Organisation Meteorologique Mondiale, 1990.

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12

Amiran, David H. K. Rainfall and water management in semi-arid climates: Israel as an example. Jerusalem Institute for Israel Studies, 1995.

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13

Ahlcrona, Eva. Monitoring the impact of climate and man on land transformation: A study in arid and semi-arid environment in Central Sudan. Department of Physical Geography, University of Lund, 1986.

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14

service), SpringerLink (Online, ed. Progressive Development: To Mitigate the Negative Impact of Global Warming on the Semi-arid Regions. Springer-Verlag Berlin Heidelberg, 2010.

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15

Wijngaarden, Willem van. Elephants, trees, grass, grazers: Relationships between climate, soils, vegetation, and large herbivores in a semi-arid savanna ecosystem (Tsavo, Kenya). International Institute for Aerospace Survey and Earth Sciences, 1985.

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16

A, Henderson-Sellers, and Pitman A. J, eds. Vegetation and climate interactions in semi-arid regions. Kluwer Academic Publishers, 1991.

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17

Henderson-Sellers, A. Vegetation and climate interactions in semi-arid regions. Ingramcontent, 2012.

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18

Craig, Ribot Jesse, Magalhães Antonio Rocha, and Panagides Stahis Solomon 1937-, eds. Climate variability, climate change, and social vulnerability in the semi-arid tropics. Cambridge University Press, 1996.

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19

(Editor), Jesse C. Ribot, Antonio Rocha Magalhães (Editor), and Stahis Panagides (Editor), eds. Climate Variability, Climate Change and Social Vulnerability in the Semi-arid Tropics. Cambridge University Press, 2005.

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20

1959-, Ribot Jesse C., Magalhães Antonio Rocha, and Panagides Stahis S. 1937-, eds. Climate variability, climate change, and social vulnerability in the semi-arid tropics. Cambridge University Press, 2005.

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21

Ribot, Jesse C., Antonio Rocha Magalhães, and Stahis Panagides, eds. Climate Variability, Climate Change and Social Vulnerability in the Semi-arid Tropics. Cambridge University Press, 1996. http://dx.doi.org/10.1017/cbo9780511608308.

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22

(Editor), A. Henderson-Sellers, and A. J. Pitman (Editor), eds. Vegetation and Climate Interactions in Semi-Arid Regions (Advances in Vegetation Science(discontinued)). 9th ed. Springer, 2007.

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23

Semi-árido: Catálogo de documentos do Instituto Otto Guerra. Editora da UFRN, 1997.

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24

Raju, K. V., and S. P. Wani. Community and Climate Resilience in the Semi-Arid Tropics: A Journey of Innovation. Springer, 2020.

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25

Esler, Karen J., Anna L. Jacobsen, and R. Brandon Pratt. Evolution and Diversity. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198739135.003.0005.

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As mediterranean-type climate (MTC) regions emerged and expanded, species from the regional pool colonized and persisted in these new climate regions. In general, taxa were derived from a few types of historical ‘geoflora’ communities: temperate forest, subtropical and tropical, and semi-arid or arid. Some of the taxa within modern mediterranean-type vegetation represent relatively ancient relict taxa that pre-date the emergence of mediterranean-type drivers. Other lineages underwent subsequent speciation, resulting in the evolution of new MTC region-specific taxa, including the production of
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26

The Impact of Climatic Variations on Agriculture : Volume 2: Assessments in Semi-Arid Regions. Springer, 2011.

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27

Parry, M. L. The Impact of Climatic Variations on Agriculture : Volume 2: Assessments in Semi-Arid Regions. Springer, 2011.

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28

Schmandt, Jurgen, Aysegül Kibaroglu, Regina Buono, and Sephra Thomas, eds. Sustainability of Engineered Rivers In Arid Lands. Cambridge University Press, 2021. http://dx.doi.org/10.1017/9781108261142.

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This interdisciplinary volume examines how nine arid or semi-arid river basins with thriving irrigated agriculture are doing now and how they may change between now and mid-century. The rivers studied are the Colorado, Euphrates-Tigris, Jucar, Limarí, Murray-Darling, Nile, Rio Grande, São Francisco, and Yellow. Engineered dams and distribution networks brought large benefits to farmers and cities, but now the water systems face multiple challenges, above all climate change, reservoir siltation, and decreased water flows. Unchecked, they will see reduced food production and endanger the economi
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29

(Editor), M. L. Parry, T. R. Carter (Editor), and N. T. Konijn (Editor), eds. The Impact of Climatic Variations on Agriculture: Volume 1: Assessments in Cool Temperate and Cold Regions Volume 2: Assessments in Semi-Arid Regions. Springer, 1988.

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30

Zeb, Aurang. Long-term effects of changes in vegetation condition, precipitation and watershed parameters on summer low-flows in the semi-arid Pacific Northwest. 1994.

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31

Zeb, Aurang. Long-term effects of changes in vegetation condition, precipitation and watershed parameters on summer low-flows in the semi-arid Pacific Northwest. 1994.

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32

G, Savenije H. H., and Matejka F, eds. Land use change and climate feedback with particular reference to the water balance of semi-arid regions. Pergamon, 1998.

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33

Xiaoling, Pan, Zhongguo hai yang xue hui., Society of Photo-optical Instrumentation Engineers., United States. National Aeronautics and Space Administration. Earth Science Technology Office., and Guo jia yao gan zhong xin (China), eds. Ecosystems dynamics, ecosystem-society interactions, and remote sensing applications for semi-arid and arid land: 24-27 October 2002, Hangzhou, China. SPIE, 2003.

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34

Filho, Walter Leal, and Josep de Trincheria Gomez. Rainwater-Smart Agriculture in Arid and Semi-Arid Areas: Fostering the Use of Rainwater for Food Security, Poverty Alleviation, Landscape Restoration and Climate Resilience. Springer, 2019.

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35

Filho, Walter Leal, and Josep de Trincheria Gomez. Rainwater-Smart Agriculture in Arid and Semi-Arid Areas: Fostering the Use of Rainwater for Food Security, Poverty Alleviation, Landscape Restoration and Climate Resilience. Springer, 2018.

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36

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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37

Climatic variability and agricultural production in central and eastern Kenya: Papers included in the Kenya case study for the assessment of climatic impacts on agriculture, semi-arid regions : a project of the International Institute for Applied Systems Analysis and the United Nations Environment Programme. National Environment Secretariat, Ministry of Environment and Natural Resources, 1985.

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38

Fensholt, Rasmus, Cheikh Mbow, Martin Brandt, and Kjeld Rasmussen. Desertification and Re-Greening of the Sahel. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.553.

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In the past 50 years, human activities and climatic variability have caused major environmental changes in the semi-arid Sahelian zone and desertification/degradation of arable lands is of major concern for livelihoods and food security. In the wake of the Sahel droughts in the early 1970s and 1980s, the UN focused on the problem of desertification by organizing the UN Conference on Desertification (UNCOD) in Nairobi in 1976. This fuelled a significant increase in the often alarmist popular accounts of desertification as well as scientific efforts in providing an understanding of the mechanism
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39

(Editor), M. L. Parry, T. R. Carter (Editor), and N. T. Konijn (Editor), eds. The Impact of Climatic Variations on Agriculture: Volume 1: Assessments in Cool Temperate and Cold Regions Volume 2: Assessments in Semi-Arid Regions. Springer, 2007.

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40

(Editor), M. L. Parry, T. R. Carter (Editor), and N. T. Konijn (Editor), eds. The Impact of Climatic Variations on Agriculture: Volume 1: Assessments in Cool Temperate and Cold Regions Volume 2: Assessments in Semi-Arid Regions. Springer, 1988.

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41

deBuys, William. A Great Aridness. Oxford University Press, 2011. http://dx.doi.org/10.1093/oso/9780199778928.001.0001.

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With its soaring azure sky and stark landscapes, the American Southwest is one of the most hauntingly beautiful regions on earth. Yet staggering population growth, combined with the intensifying effects of climate change, is driving the oasis-based society close to the brink of a Dust-Bowl-scale catastrophe. In A Great Aridness, William deBuys paints a compelling picture of what the Southwest might look like when the heat turns up and the water runs out. This semi-arid land, vulnerable to water shortages, rising temperatures, wildfires, and a host of other environmental challenges, is poised t
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42

Holmes, Jonathan, and Philipp Hoelzmann. The Late Pleistocene-Holocene African Humid Period as Evident in Lakes. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.531.

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From the end of the last glacial stage until the mid-Holocene, large areas of arid and semi-arid North Africa were much wetter than present, during the interval that is known as the African Humid Period (AHP). During this time, large areas were characterized by a marked increase in precipitation, an expansion of lakes, river systems, and wetlands, and the spread of grassland, shrub land, and woodland vegetation into areas that are currently much drier. Simulations with climate models indicate that the AHP was the result of orbitally forced increase in northern hemisphere summer insolation, whi
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43

Lachniet, Matthew S., and Juan Pablo Bernal-Uruchurtu. AD 550–600 Collapse at Teotihuacan. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780199329199.003.0006.

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We analyze a 2400-year rainfall reconstruction from an ultra-high-resolution absolutely-dated stalagmite (JX-6) from southwestern Mexico (Lachniet et al., 2012). Oxygen isotope variations correlate strongly to rainfall amount in the Mexico City area since 1870 CE, and for the wider southwestern Mexico region since 1948, allowing us to quantitatively reconstruct rainfall variability for the Basin of Mexico and Sierra Madre del Sur for the past 2400 years. Because oxygen isotopes integrate rainfall variations over broad geographic regions, our data suggest substantial variations in Mesoamerican
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