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Author: Grafiati
Published: 10 December 2022
Last updated: 28 January 2023

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1

Fay, Marianne. Adapting to climate change in Eastern Europe and Central Asia. Washington, DC: World Bank, 2010.

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2

Rachel, Block, and Ebinger Jane O, eds. Adapting to Climate change in Eastern Europe and Central Asia. Washington DC: World Bank, 2010.

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3

Glantz, Michael H. The Aral Sea: Water, climate, and environmental change in Central Asia. [Geneva]: World Meteorological Organization, 2005.

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4

GCOS Regional Workshop for Central Asia on Improving Observing Systems for Climate (2004 Almaty, Kazakhstan). Report of the GCOS Regional Workshop for Central Asia on Improving Observing Systems for Climate: Almaty, Kazakhstan, 24-26 May 2004. Geneva, Switzerland: GCOS Secretariat, Global Climate Observing System, 2005.

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5

Srivastava, Jitendra, William R. Sutton, and James E. Neumann. Looking beyond the horizon: How climate change impacts and adaptation responses will reshape agriculture in Eastern Europe and Central Asia. Washington, D.C: World Bank, 2013.

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6

Corrêa, P. H. da Rocha. Technology adoption and the investment climate: Firm-level evidence for Eastern Europe and Central Asia. [Washington, D.C: World Bank, 2008.

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7

1935-, Agrawal D. P., Kusumgar Sheela 1939-, and Krishnamurthy R. V, eds. Climate and geology of Kashmir, the last 4 million years: Proceedings of the International Workshop on the Late Cenozoic Palaeoclimatic Changes in Kashmir and Central Asia, Ahmedabad, 19-23 October 1982. New Delhi: Today & Tomorrow's Printers and Publishers, 1985.

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8

Hartmut, Vogtmann, Dobret︠s︡ov Nikolaĭ Leontʹevich, Mittelstaedt Astrid, and NATO Public Diplomacy Division, eds. Environmental security and sustainable land use: With special reference to Central Asia. Dordrecht: Springer in cooperation with NATO Public Diplomacy Division, 2006.

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9

Climate Finance Toolkit for Europe and Central Asia. FAO, 2021. http://dx.doi.org/10.4060/cb6933en.

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10

Climate Finance Toolkit for Europe and Central Asia. FAO, 2021. http://dx.doi.org/10.4060/cb6933en.

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11

Celikyilmaz, G., and C. Arguello. Climate Finance Toolkit for Europe and Central Asia. Food & Agriculture Organization of the United Nations, 2022.

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12

Agarwal, D. P., and Sheela Kusumgar. Climate and Geology of Kashmir and Central Asia (Current Trends in Geology, Vol 6). Scholarly Pubns, 1985.

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13

R, Lal, ed. Climate change and terrestrial carbon sequestration in Central Asia. Boca Raton, FL: Taylor & Francis, 2007.

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14

Stewart, B. A., Rattan Lal, M. Suleimenov, D. O. Hansen, and Paul Doraiswamy. Climate Change and Terrestrial Carbon Sequestration in Central Asia. Taylor & Francis Group, 2007.

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15

Stewart, B. A., R. Lal, M. Suleimenov, D. O. Hansen, and Paul C. Doraiswamy. Climate Change and Terrestrial Carbon Sequestration in Central Asia. Taylor & Francis Group, 2019.

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16

Carmin, JoAnn, and Yan Zhang. Achieving Urban Climate Adaptation In Europe And Central Asia. The World Bank, 2009. http://dx.doi.org/10.1596/1813-9450-5088.

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17

Stewart, B. A., Rattan Lal, M. Suleimenov, D. O. Hansen, and Paul Doraiswamy. Climate Change and Terrestrial Carbon Sequestration in Central Asia. Taylor & Francis Group, 2007.

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18

Stewart, B. A., Rattan Lal, M. Suleimenov, D. O. Hansen, and Paul Doraiswamy. Climate Change and Terrestrial Carbon Sequestration in Central Asia. Taylor & Francis Group, 2007.

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19

(Editor), Rattan Lal, M. Suleimenov (Editor), B. A. Stewart (Editor), D. O. Hanson (Editor), and P. Doraiswamy (Editor), eds. Climate Change and Terrestrial Carbon Sequestration in Central Asia. CRC, 2007.

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20

Stewart, B. A., Rattan Lal, M. Suleimenov, D. O. Hansen, and Paul Doraiswamy. Climate Change and Terrestrial Carbon Sequestration in Central Asia. Taylor & Francis Group, 2007.

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21

Weather and Climate Services in Europe and Central Asia. The World Bank, 2008. http://dx.doi.org/10.1596/978-0-8213-7585-3.

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22

Stewart, B. A., Rattan Lal, M. Suleimenov, D. O. Hansen, and Paul Doraiswamy. Climate Change and Terrestrial Carbon Sequestration in Central Asia. Taylor & Francis Group, 2007.

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23

Stewart, B. A., Rattan Lal, M. Suleimenov, D. O. Hansen, and Paul Doraiswamy. Climate Change and Terrestrial Carbon Sequestration in Central Asia. Taylor & Francis Group, 2007.

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24

Bank, Asian Development. Economics of Climate Change Mitigation in Central and West Asia. Asian Development Bank Institute, 2017.

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25

Improving Weather, Climate, and Hydrological Services Delivery in Central Asia. World Bank, Moscow, 2016. http://dx.doi.org/10.1596/23777.

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26

Oral, Isil, Indhira Santos, and Fan Zhang. Climate Change Policies and Employment in Eastern Europe and Central Asia. The World Bank, 2012. http://dx.doi.org/10.1596/1813-9450-6294.

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27

Financing Climate Action in Eastern Europe, the Caucasus and Central Asia. OECD, 2016. http://dx.doi.org/10.1787/9789264266339-en.

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28

Bank, World, ed. Weather and climate services in Europe and Central Asia: A regional review. Washington, D.C: World Bank, 2008.

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29

Organisation for economic co-operation and development. Financing Climate Action in Eastern Europe, the Caucasus and Central Asia (Russian Version). Organization for Economic Cooperation & Development, 2017.

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30

Larson, Donald F., Ariel Dinar, and Brian Blankespoor. Aligning Climate Change Mitigation and Agricultural Policies in Eastern Europe and Central Asia. The World Bank, 2012. http://dx.doi.org/10.1596/1813-9450-6080.

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31

Financing Climate Action in Eastern Europe, the Caucasus and Central Asia (Russian version). OECD, 2017. http://dx.doi.org/10.1787/9789264286047-ru.

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32

Gerling, Kerstin, Yasser Abdih, Christoph Duenwald, Vahram Stepanyan, and Abdullah Al-Hassan. Feeling the Heat: Adapting to Climate Change in the Middle East and Central Asia. International Monetary Fund, 2022.

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33

Gerling, Kerstin, Yasser Abdih, Christoph Duenwald, Vahram Stepanyan, and Abdullah Al-Hassan. Feeling the Heat: Adapting to Climate Change in the Middle East and Central Asia. International Monetary Fund, 2022.

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34

Gerling, Kerstin, Yasser Abdih, Christoph Duenwald, Vahram Stepanyan, and Abdullah Al-Hassan. Feeling the Heat: Adapting to Climate Change in the Middle East and Central Asia. International Monetary Fund, 2022.

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35

OECD. Green Finance and Investment Financing Climate Action in Eastern Europe, the Caucasus and Central Asia. Organization for Economic Cooperation & Development, 2016.

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36

On The Frontiers Of Climate And Environmental Change Vulnerabilities And Adaptations In Central Vietnam. Springer-Verlag Berlin and Heidelberg GmbH &, 2013.

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37

Correa, Paulo G., Ana M. Fernandes, and Chris J. Uregian. Technology Adoption And The Investment Climate: Firm-Level Evidence For Eastern Europe And Central Asia. The World Bank, 2008. http://dx.doi.org/10.1596/1813-9450-4707.

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38

Climate change impacts on twenty major crop pests in Central Asia, the Caucasus and Southeastern Europe. FAO;, 2021. http://dx.doi.org/10.4060/cb5954en.

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39

Agarwal, D. P. Climate and Geology of Kashmir and Central Asia ; The Last 4 Million Years : Proceedings of the International Workshop on the Late Cenozoic Palaeoclimatic Changes in Kashmir and Central Asia, Ahmedaba. Today & Tomorrow's Printers and Publishe, 1985.

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40

Weninger, Bernhard, and Lee Clare. 6600–6000 cal BC Abrupt Climate Change and Neolithic Dispersal from West Asia. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780199329199.003.0003.

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Recent advances in palaeoclimatological and meteorological research, combined with new radiocarbon data from western Anatolia and southeast Europe, lead us to formulate a new hypothesis for the temporal and spatial dispersal of Neolithic lifeways from their core areas of genesis. The new hypothesis, which we term the Abrupt Climate Change (ACC) Neolithization Model, incorporates a number of insights from modern vulnerability theory. We focus here on the Late Neolithic (Anatolian terminology), which is followed in the Balkans by the Early Neolithic (European terminology). From high-resolution 14C-case studies, we infer an initial (very rapid) west-directed movement of early farming communities out of the Central Anatolian Plateau towards the Turkish Aegean littoral. This move is exactly in phase (decadal scale) with the onset of ACC conditions (~6600 cal BC). Upon reaching the Aegean coastline, Neolithic dispersal comes to a halt. It is not until some 500 years later—that is, at the close of cumulative ACC and 8.2 ka cal BP Hudson Bay cold conditions—that there occurs a second abrupt movement of farming communities into Southeast Europe, as far as the Pannonian Basin. The spread of early farming from Anatolia into eastern Central Europe is best explained as Neolithic communities’ mitigation of biophysical and social vulnerability to natural (climate-induced) hazards.
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41

Benecke, Norbert. Subsistence economy, animal domestication, and herd management in prehistoric central Asia (Neolithic–Iron Age). Edited by Umberto Albarella, Mauro Rizzetto, Hannah Russ, Kim Vickers, and Sarah Viner-Daniels. Oxford University Press, 2017. http://dx.doi.org/10.1093/oxfordhb/9780199686476.013.21.

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Sites of the Neolithic Jeitun Culture in southern Turkmenistan present the earliest evidence of animal husbandry, mainly based on sheep (Ovis aries) and goats (Capra hircus), in Central Asia. In its northern parts, subsistence economy relied on the exploitation of wild animal resources in the Neolithic and Chalcolithic. The steppes of north Kazakhstan played a prominent role in the domestication of the horse (Equus caballus) some time prior to 3000 bc. In subsequent periods, horse breeding was of great economic importance in this area. In the Bronze Age, the Bactrian camel (Camelus bactrianus) became a common livestock animal in the Eurasian dry zones. Its domestication seems to have taken place in the southwestern part of Central Asia. According to geography, vegetation, and climate, different types of animal keeping and herd management developed in the centuries of the Bronze and Iron Ages.
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42

Yang, Kun. Observed Regional Climate Change in Tibet over the Last Decades. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.587.

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The Tibetan Plateau (TP) is subjected to strong interactions among the atmosphere, hydrosphere, cryosphere, and biosphere. The Plateau exerts huge thermal forcing on the mid-troposphere over the mid-latitude of the Northern Hemisphere during spring and summer. This region also contains the headwaters of major rivers in Asia and provides a large portion of the water resources used for economic activities in adjacent regions. Since the beginning of the 1980s, the TP has undergone evident climate changes, with overall surface air warming and moistening, solar dimming, and decrease in wind speed. Surface warming, which depends on elevation and its horizontal pattern (warming in most of the TP but cooling in the westernmost TP), was consistent with glacial changes. Accompanying the warming was air moistening, with a sudden increase in precipitable water in 1998. Both triggered more deep clouds, which resulted in solar dimming. Surface wind speed declined from the 1970s and started to recover in 2002, as a result of atmospheric circulation adjustment caused by the differential surface warming between Asian high latitudes and low latitudes.The climate changes over the TP have changed energy and water cycles and has thus reshaped the local environment. Thermal forcing over the TP has weakened. The warming and decrease in wind speed lowered the Bowen ratio and has led to less surface sensible heating. Atmospheric radiative cooling has been enhanced, mainly through outgoing longwave emission from the warming planetary system and slightly enhanced solar radiation reflection. The trend in both energy terms has contributed to the weakening of thermal forcing over the Plateau. The water cycle has been significantly altered by the climate changes. The monsoon-impacted region (i.e., the southern and eastern regions of the TP) has received less precipitation, more evaporation, less soil moisture and less runoff, which has resulted in the general shrinkage of lakes and pools in this region, although glacier melt has increased. The region dominated by westerlies (i.e., central, northern and western regions of the TP) received more precipitation, more evaporation, more soil moisture and more runoff, which together with more glacier melt resulted in the general expansion of lakes in this region. The overall wetting in the TP is due to both the warmer and moister conditions at the surface, which increased convective available potential energy and may eventually depend on decadal variability of atmospheric circulations such as Atlantic Multi-decadal Oscillation and an intensified Siberian High. The drying process in the southern region is perhaps related to the expansion of Hadley circulation. All these processes have not been well understood.
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43

Kovács, Antal Ferenc. Green Financial Perspectives - Proceeds of the Central European Scientific Conference on Green Finance and Sustainable Development, October 2020. Edited by Géza Salamin. Corvinus University of Budapest, 2021. http://dx.doi.org/10.14267/978-963-503-890-9.

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This publication presents eleven selected articles in two thematic chapters. The chapter titled Institutions and Instruments is focused on the role of institutions, among them the central banks, as well as various financial instruments designed to pursue sustainability at the micro-level, such as corporate reporting on environmental, social and governance performance (ESG), the pricing of carbon, and performance of stock exchange listed shares etc.. The wealth perspective is presented as a framework that offers a comprehensive approach to the issue of sustainability. Articles in the second chapter provide climate and sustainability insights at the macro level in the regions of Central-Asia, the Middle-East and Europe.
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44

Tasar, Eren. Epilogue. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780190652104.003.0008.

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Dramatic changes took place in the religious sphere during the tumultous final years of Soviet history. Shamsuddin Boboxonov’s unprecedented ouster as mufti in 1989 offered a preview of the confusion that was to come: SADUM’s disintegration into national muftiates for each of the five Central Asian republics took place rapidly, in a climate of ethnic conflict. Though the Central Asian muftiate ceased to exist in 1991, the precedents established by the CRA-SADUM alliance continued to shape relations between Islam and the state in the post-Soviet period. In one important respect, however, those relations have departed dramatically from the Soviet legacy: now that the independent republics have abandoned communism and atheism, little incentive exists for a moderate line toward religion. This explains why state policies toward religion in post-Soviet Central Asia became more repressive after the collapse of the USSR, not less.
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45

Fay, Marianne, Rachel I. Block, and Jane Ebinger, eds. Adapting to Climate Change in Eastern Europe and Cental Asia. The World Bank, 2010. http://dx.doi.org/10.1596/978-0-8213-8131-1.

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46

Project, Baikal Drilling, ed. International project, "The Baikal Drilling Project": International investigations of the paleolimnological and tectonic development of the Baikal rift structure in terms of the international program "Global changes of the environment and climate in Central Asia based on sedimentological studies of Lake Baikal", Russia, U.S.A., Japan. [Russia: s.n., 1993.

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47

Perdue, Peter C. Owen Lattimore. Oxford University Press, 2018. http://dx.doi.org/10.1093/oxfordhb/9780199935369.013.26.

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The American scholar, traveler, political adviser, and public intellectual Owen Lattimore strongly shaped American public opinion toward China and Central Eurasia in the twentieth century, but he also wrote major works on the geography and environment of the frontiers of Asia that still influence global historians today. His writings asserted the vital importance of China’s relationship with the nomads of the steppe, including the Mongols, for defining the boundaries, cultures, and geopolitical strategy of empires and nation states. He argued for sophisticated explanations of relationships between environmental forces like climate and human culture, and he analyzed China and Central Eurasia so as to provide new perspectives on world history. This article evaluates Lattimore’s contributions to world history in the light of his dynamic political and academic life.
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48

Goodrich, Chanda Gurung, Dibya Devi Gurung, and Aditya Bastola. State of gender equality and climate change in Nepal. International Centre for Integrated Mountain Development (ICIMOD), 2021. http://dx.doi.org/10.53055/icimod.790.

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The State of Gender Equality and Climate Change is a series of reports covering countries across the Asia-Pacific (Vietnam and Cambodia), and Nepal. The report raises awareness about the need for gender-responsive climate action, analyzes gendered impacts of climate change, and suggests ways to enhance and mainstream gender equality into climate-relevant sectoral policies and actions. The objectives of the report are two-fold: 1. To strengthen country-driven processes by presenting more evidence of the links between gender equality and climate change and analysing gendered impacts in the forestry, agriculture, energy, and water sectors; and 2. To provide country-specific recommendations on enhancing gender responsive policy implementation and actions to further augment the integration of gender equality in climate relevant policy areas. The Nepal country report was prepared by the International Centre for Integrated Mountain Development (ICIMOD), United Nations Environment Programme (UNEP), and UN Women.
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49

Environmental Security and Sustainable Land Use - with special reference to Central Asia (NATO Science for Peace and Security Series / NATO Science for ... Security Series C: Environmental Security). Springer, 2006.

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50

(Editor), Hartmut Vogtmann, and Nikolai Dobretsov (Editor), eds. Environmental Security and Sustainable Land Use - with special reference to Central Asia (NATO Science for Peace and Security Series / NATO Science for ... Security Series C: Environmental Security). Springer, 2006.

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