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Article

Consideration of Water Uses for Its Sustainable Management, the Case of Issyk-Kul Lake, Kyrgyzstan

by
Burul Alymkulova
1,2,3,*,
Jilili Abuduwaili
1,3,*,
Gulnur Issanova
3,4 and
Lamek Nahayo
1,5
1
State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, 818 South Beijing Road, Urumqi 830011, Xinjiang, China
2
University of Chinese Academy of Sciences, Beijing 10049, China
3
CAS Research Center for Ecology and Environment of Central Asia, Urumqi 830011, Xinjiang, China
4
Research Centre of Ecology and Environment of Central Asia, Al-Farabi Kazakh National University, Almaty 050040, Kazakhstan
5
Faculty of Environmental Studies, University of Lay Adventists of Kigali, POB Box 6392, Kigali, Rwanda
*
Authors to whom correspondence should be addressed.
Water 2016, 8(7), 298; https://doi.org/10.3390/w8070298
Submission received: 17 May 2016 / Revised: 29 June 2016 / Accepted: 9 July 2016 / Published: 19 July 2016

Abstract

:
Water is an essential element for life, and development would not be possible without its availability. This study identified the main water consumers and their likely impact on water lake level for the case of Issyk-Kul Lake Basin, Kyrgyzstan. Data on precipitation, lake level, irrigation, household and industrial water consumption from 1980 to 2014 were provided by the Department of Water Resources and Irrigation, Ministry of Agriculture and Land Reclamation of the Kyrgyz Republic. The input data was analyzed with OriginPro 8.5 for Statistical Analysis. The results indicated a decreasing irrigation water consumption from 2029.42 to 461.76 million·m3 in 1980 and 2014, respectively. Likewise, households consumed 27.02 million·m3 in 1980 falling to 16.55 million·m3 in 2014, similar to the manufacture’s water consumption. However, it was noted that agriculture is a high water consumer, whose water demand for irrigation rises from April to August, the period during which the precipitation also increases. Nevertheless, manufactures and household water consumption do not have timed limits of use like in agriculture, which in turn affects the lake water level. Therefore, as the rainfall increases by April to August, we suggest to harvest and only use the rainfall water during its abundance period. This would help in restoring the lake’s water level during the time of rainwater uses, and leads to water consumption balance, flood management and lake biodiversity conservation as well.

Graphical Abstract

1. Introduction

Agricultural irrigation practices, rapid urbanization and climate change increase pressure on water resources. The world population is projected to be 9.7 billion by 2050, an increase of about 2 billion from today (7 billion); this world population may increase its pressure on both water quality and quantity [1,2]. Worldwide water utilities experience seasonal fluctuations in their aggregate consumption levels and these variations generally cause specialized maintenance and administrative schedules to develop individual utilities as a mean of optimizing the natural resources [3]. Water from rivers, lakes and aquifers is mostly used for irrigation, bathing, washing and other human needs. Increasing exploitation of natural resources, inappropriate land-use practices, and uncoordinated sectoral policies and development activities in lake basins impair various important functions of water. Therefore, appropriate approaches for water management are urgently needed [4,5,6].
Natural forces and human activities have been reported to damage water resources. Despite increasing public awareness on the role of water in human health and development, water scarcity and pollution is experienced due to lack of consistency and consensus of economic and political willingness on water resources management [7,8]. Water plays an important role in the productive process, since this natural resource can become either a limiting factor for development or the driving force behind economic growth. Therefore, it is necessary to know the situation regarding water resources and its relationship with the regional productive process [9]. Water size and salinity fluctuate whenever the balance between hydrological inputs (precipitation, surface runoff and groundwater inflows) and outputs (evaporation and seepage losses) changes due to seasonal and climatic variation or anthropogenic activities [10,11]. While the impact of water diversions for irrigated agriculture and urban consumption on several large salt lakes (Aral Sea, Dead Sea, Mono Lake) has been widely publicized, the global extent and rapidity with which saline lakes are being impacted throughout the world has yet to be fully appreciated [12,13].
Kyrgyzstan is a Central Asian country with the advantage of having water resources fully formed in its own territory. Kyrgyzstan has significant resources of underground and surface waters, stocks of which are in the rivers, glaciers and eternal snow arrays. The country has more than 3500 rivers and streams, which belong to the main pools; the Syr-Darya river, the Amu Darya, Chu, Talas, Tarim and Lake Issyk-Kul [14,15,16]. On its territory is the the Issyk-Kul basin formed by a plurality of streams, of which about 123 are used for irrigation purposes. Surface water is characterized by sediment, salts and fine sediments transported by the lake surrounding rivers. Mineralization of surface waters in general is less than 1 g/L, which makes it suitable for irrigation [17,18]. The Lake Issyk-Kul has been subject to changes in its water level, increasing sediments and other anthropogenic activities which changed its physical-chemical properties [19]. Previous studies conducted at Lake Issyk-Kul [18,20,21] have identified its main problems related to water pollution and its increasing water demand, which in turn, threaten sustainable use of the lake, fisheries, glacial retreat, agriculture, water diversions, biodiversity, tourism and its biosphere reserve. This shows that Issyk-Kul Lake Basin is under increasing pressure which needs accurate and sustainable management for its continuous use. Therefore, the objectives of this study are to (1) consider historical water consumption and its main users and (2) provide suggestions, based on the results, regarding how the lake water can be sustainably productive and usable.

2. Materials and Methods

2.1. Description of the Study Area

Issyk-Kul lake basin is a closed mountain lake, located at about 77° E and 42°30′ N, in the northern part of the Tian-Shan mountain belt in the Kyrgyz Republic (Central Asia). It is situated at an altitude of 1607 m above sea level and surrounded by high mountain ranges: the Kungey Ala-Too Range in the north with the highest peaks reaching 4770 m, and the Teskey Ala-Too Range in the south with peaks exceeding 5200 m [22,23,24], see in Figure 1. The total area equals approximately 22,080 km2, of which the lake occupies 6236 km2, the coastal zone called zone dissipation runoff occupies 3092 km2, and other part of the basin (12,752 km2) is occupied by mountain areas.
Moreover, about 118 rivers enter the lake and are predominantly fed by melt-water from snow and glaciers, which occupy about 509 km2 of this drainage basin, at altitudes of 3000 m and above [25,26,27]. Currently, 17 hydrological stations are in use around the lake. The main local lake’s climate formation factors are a huge mass of water and the chain mountainous ridges that protect the basin from the scorching breath of the Central Asian deserts. The climate of Issyk-Kul basin is moderately warm, favorable for grain, crops and gardening [28,29].

2.2. Data Collection and Analysis

This study used data on irrigation, household and manufactures water consumption and lake water level provided by the Department of Water Resources and Irrigation, Ministry of Agriculture and Land Reclamation of the Kyrgyz Republic, from 1980 to 2013. Data on precipitation was provided by the Meteorological stations (Cholpon-Ata, Balykchy, Kyzyl-Suu and Karakol) located around the Issyk-Kul Lake Basin. The input data was analyzed with OriginPro 8.5 for Statistical analysis. In addition, this study adopted the literature methodology to facilitate the analysis and discussion of the results.

3. Results

3.1. Issyk-Kul Lake Water Level and Supply

Issyk-Kul Lake has been subject to several water consumers, including but not limited to construction, irrigation and recreation. These water uses led to variation in the lake’s water level being headed by agricultural irrigation water demand, which was 43% in 1998 of the total lake tributaries [19], against today’s increase, which is more than 70% compared to other lake’s water consumers.
As indicated in Figure 2, the lake registered little seasonal variation of water levels from 1606.73 m in 1980 to 1606.29 m in 1999, while from 2000, the water level slightly increased until 2011 (1607.02 m) and ended in 2012 with small decreasing numbers (1606.99 m). These alterations of water level can result from the lake water uses and the system under which the water is used and/or climate change, which is reported to affect water resources.

3.2. Annual Precipitation Variation

The Issyk-Kul lake water is subject to changes in the runoff and distribution of its sources, mainly the rainfall, snowmelt water, glaciers and other tributaries. However, as indicated in Figure 3 below, some years feature heavy precipitation compared to others, which in turn affects the lake water level. The precipitation was marked by increasing and decreasing records. The high value was registered in 1993 (35 mm) and the lowest was 12.3 mm in 1997, while the years of 2007 up to 2013 recorded decreasing rainfall from about 29.9 to 25 mm, respectively.

3.3. Main Issyk-Kul Lake Water Consumers

The results (Table 1) on the lake’s water consumers considered (agricultural irrigation, manufacture and household) from 1980 to 2014 reveal decreasing water consumption numbers. This reduction in water consumption could be a result of the collapse of the Soviet Union in 1989–1992, where water users decreased and the remaining were deployed in different places, meaning that they used other water sources [29,30]. However, as the population around the lake grows, its water demand rises, and leads to a water level decrease, which was detected and controlled by government policies through using other lakes and basins, managing the lake’s streams, soil erosion control measures, rainwater harvesting, etc. [17,19,26,31].
Although agriculture water demand showed decreasing numbers (Table 1), its water demand has been reported [8,32] to change over time with great likelihood of increasing water demand depending on the type of crops grown. In addition, the types of irrigation like flooding or sprinkler cause high volume water consumption, because they are associated with environmental effects like water salinization, while, drip irrigation is suggested for both quantity and quality of water management, as it does not consume much water but helps to reach crops with minimum total water use [33,34]. Therefore, it is good to consider the best irrigation practices which favor water management at Issyk-Kul Lake Basin.

4. Discussion

4.1. Water Resources and Increasing Demand

Issyk-Kul has been subject to changes in its water level, increasing sediments and other anthropogenic activities such as expansion of agricultural irrigated lands and rise of recreational, household and industrial water demand [18,20,21]. These threaten the lake fisheries, glacial, water quality, biodiversity, biosphere and other socio-economic and environmental services and call for appropriate measures for its sustainable management and use.
Water demand at Issyk-Kul Basin Lake (Table 1), reveals decreasing numbers, which could be a result of the region’s background and the lake water management measures adopted [29,30]. However, as the basin is used for many other purposes, such as ecological or socio-economic [20,31]. This exposes the lake to natural and anthropogenic forces, meaning that whatever measures are taken for its management, there is great need to consider each and every demand and/or use to sustainably manage the lake water due to its role in the sustainable socio-economic development of the region.

4.2. Climate Change and Water

Climate change puts pressure on the quantity and quality of water resources. This pressure has been previously reported to lead to precipitation fluctuations in Asian countries [8,35,36] and these shifts on the hydrological budget are expected to increase with effect on water resources.
The findings, illustrated in Figure 4 below, are in agreement with previous findings [37,38] that highlighted how variation in precipitation is among reasons of water shortage, and suggested using rainfall harvest as an alternative and involving local community, who the most affected by water deficit, in decision making regarding water resources management. This enhances durable access to safe and clean water and its management, and ensures that everyone involved will consider the right way of sustainably using water [39].
In addition, precipitation increases from April to July/August, then keeps on decreasing up to the end of the year (Figure 5), while in October, agricultural water demand rises again (Figure 4), under decreasing precipitation. This shows that the time of high volume of water demand is not proportional with its availability (Figure 4 against Figure 5), which can be seen in previous studies [33,40] which reported that agriculture is among the world’s most significant water consumers and its water consumption is projected to keep increasing as long as the human population grows, where adaptive policies are to be regarded. Moreover, the population located near Issyk-Kul Lake grew from 441.3 to 458.5 thousand in 2010 and 2014, respectively [41]. This expresses increasing food demand, household and other development activities which require availability and access to water. For the problem to be dealt with, it is proposed to interchangeably use the lake and rainfall water [42,43].
Despite the fact that integrated water resources management action is being taken, it is still mandatory to consider climate change, global population growth and other increasing water demands for its sustainable management [44]. Furthermore, even though the results of this study revealed decreasing water demand (Table 1), to mitigate and adapt to the impact of climate change on water resources, particularly at Issyk-Kull basin, it is good to consider the hydrological weather related changes that are appearing (Figure 3 and Figure 5) and adapt accordingly.

4.3. Water and Sustainability

Sustainable development, socio-economic development, healthy ecosystem and human survival are rooted in water availability. Water helps in hosting and preserving development activities upon which human depend in daily life. It also serves as the link between the climate system, environment and human society [45,46]. Water, if efficiently and equitably managed, can help to achieve sustainable development. However, it has been reported that water scarcity is among the most significant development challenges worldwide, and access to water is not equal [47,48].
The United Nation’s (UN) overarching goal is to secure sustainable water for all, due to the role of water in ensuring people’s health, prosperity, resilient communities, equitable societies and protected ecosystems, which in turn are the basis of sustainable development [49]. Nevertheless, this cannot be realized without universal access to water, its sustainable management and effective governance [50]. Water management is also a serious problem in Eastern Asia, where a number of problems, compounding the issue include but not limited to floods, increased salinization and a loss of fresh water reserves due to agriculture along with pollution from sewage and industry have severely damaged the water supply with dangerous effects on the health of local people [51].
For sustainable management of Issyk-Kul Basin Lake, whose water is used for many purposes, there is great need to take into consideration: variation of water resources (Figure 2); the changing climate which causes fluctuations in intensity and frequency of precipitation (Figure 3 and Figure 5), one of the sources of the lake’s water; managing the changes (increase/decrease) in the demand and uses of the lake water (Figure 4 and Table 1) along with decision makers and common community understanding on the use, conservation and protection of the lake.

5. Conclusions

This study considered the Issyk-Kul Lake to determine the change in its water consumption and suggest future water management practices. The results indicated that agriculture was the main water consumer for irrigation practices along with household and manufacture water consumption. The identified lake water consumers revealed decreasing numbers; however, meteorological stations and annual average precipitation indicated timely variation in rainfall, one of the lake water sources. Precipitation increases from May to July and/or August, the period in which agricultural water demand (seasonal) was increasing. This can lead to drought if consumers use lake water and/or flooding due to heavy rain which is not managed. Based on the findings for water management at Issyk-Kull lake, we suggest to (1) consider maximum rainfall harvest for the lake water and biodiversity conservation; (2) irrigate with the rainfall water during its falling time and reserve the lake water for manufacture and households whose water demand does not have a time limit; and finally (3) integrate decision makers and the local community (water users) into water resources management policy making.

Acknowledgments

The authors would like to gratefully thank the Science and Technology Service Network Fund Project in Chinese Academy of Sciences (TSS-2015-014-FW-1-2), the National Natural Science Foundation of China (41471098), the International Science and Technology Cooperation Program of China (2010DFA92720) and the Foundation of State Key Laboratory of Desert and Oasis Ecology for funding this research and the Department of Water Resources and Irrigation, Ministry of Agriculture and Land Reclamation of the Kyrgyz Republic for the provision of data.

Author Contributions

Burul Alymkulova and Jilili Abuduwaili designed the study; Gulnur Issanova statistically computed the input data; Burul Alymkulova and Lamek Nahayo wrote the manuscript. Finally, all authors contributed to the final version of manuscript by proofreading.

Conflicts of Interest

The authors declare no conflict of interest.

References

  1. Wilson, J.R.; Holst, N.; Rees, M. Determinants and patterns of population growth in water hyacinth. Aquat. Bot. 2005, 81, 51–67. [Google Scholar] [CrossRef]
  2. Vörösmarty, C.J.; Green, P.; Salisbury, J.; Lammers, R.B. Global water resources: Vulnerability from climate change and population growth. Science 2000, 289, 284–288. [Google Scholar] [CrossRef] [PubMed]
  3. Fullerton, T.M.; Elias, A. Short-term water consumption dynamics in El Paso, Texas. Water Resour. Res. 2004, 40. [Google Scholar] [CrossRef]
  4. Rost, S.; Gerten, D.; Bondeau, A.; Lucht, W.; Rohwer, J.; Schaphoff, S. Agricultural green and blue water consumption and its influence on the global water system. Water Resour. Res. 2008, 44. [Google Scholar] [CrossRef]
  5. Avramoski, O. The Role of Public Participation and Citizen Involvement in Lake Basin Management. Available online: http://www.worldlakes.org/uploads/Thematic_Paper_PP_16Feb04.pdf (assessed on 14 April 2004).
  6. Koop, S.H.; van Leeuwen, C.J. Assessment of the sustainability of water resources management: A critical review of the city blueprint approach. Water Resour. Manag. 2015, 29, 5649–5670. [Google Scholar] [CrossRef]
  7. Kundzewicz, Z.W.; Mata, L.J.; Arnell, N.W.; Döll, P.; Jimenez, B.; Miller, K.; Oki, T.; Şen, Z.; Shiklomanov, I. The implications of projected climate change for freshwater resources and their management. Hydrol. Sci. J. 2008, 53, 3–10. [Google Scholar] [CrossRef]
  8. Piao, S.; Ciais, P.; Huang, Y.; Shen, Z.; Peng, S.; Li, J.; Zhou, L.; Liu, H.; Ma, Y.; Ding, Y.; et al. The impacts of climate change on water resources and agriculture in China. Nature 2010, 467, 43–51. [Google Scholar] [CrossRef] [PubMed]
  9. Velazquez, E. An input–output model of water consumption: Analysing intersectoral water relationships in Andalusia. Ecol. Econ. 2006, 56, 226–240. [Google Scholar] [CrossRef]
  10. Jellison, R.; Zadereev, Y.S.; DasSarma, P.A.; Melack, J.M.; Rosen, M.R.; Degermendzhy, A.G.; DasSarma, S.; Zambrana, G. Conservation and Management Challenges of Saline Lakes: A Review of Five Experience Briefs. Lake Basin Management Initiative: Thematic Paper. Available online: http://citeseerx.ist.psu.edu/viewdoc/download?doi=10.1.1.552.9109&rep=rep1&type=pdf (assessed on 14 July 2016).
  11. Ramana, R.V.; Krishna, B.; Kumar, S.R.; Pandey, N.G. Monthly rainfall prediction using wavelet neural network analysis. Water Resour. Manag. 2013, 27, 3697–3711. [Google Scholar] [CrossRef]
  12. Polunin, N.V.C. Aquatic Ecosystems: Trends and Global Prospects; Cambridge University Press: Cambridge, UK, 2008; pp. 94–110. [Google Scholar]
  13. Atadjanov, S.; Tulegabylov, N.; Bekkulova, D.; Baidakova, N.; Grebnev, V. The National Report on the State of the Environment of the Kyrgyz Republic for 2006–2011; United Nations Development Programme (UNDP): New York, NY, USA, 2012. [Google Scholar]
  14. Klerx, J.; Imanackunov, B. Lake Issyk-Kul: Its Natural Environment; Springer Science & Business Media: Berlin, Germany, 2002; Volume 13. [Google Scholar]
  15. Mamatkanov, D.M.; Bazhanov, L.V.; Romanovsky, V.V. Water Resources of Kyrgyzstan in Modern Days; Ilim: Bishkek, Kyrgyz Republic, 2006. [Google Scholar]
  16. Asykulov, T. The Socio-Economics and Natural Environment of Eastern Kyrgyzstan and Development Issues of Biosphere Reserve Issyk-Kul. Ph.D. Thesis, University Graysvald, Graysvald, Germany, 2002. [Google Scholar]
  17. Giralt, S.; Klerkx, J.; Riera, S.; Julia, R.; Lignier, V.; Beck, C.; De Batist, M.; Kalugin, I. Recent Paleoenvironmental Evolution of Lake Issyk-Kul, in Lake Issyk-Kul: Its Natural Environment; Springer: Berlin, Germany, 2002; pp. 125–145. [Google Scholar]
  18. Vollmer, M.K.; Weiss, R.F.; Schlosser, P.; Williams, R.T. Deep-water renewal in Lake Issyk-Kul. Geophys. Res. Lett. 2002, 29. [Google Scholar] [CrossRef]
  19. Gavshin, V.M.; Sukhorukov, F.V.; Bobrov, V.A.; Melgunov, M.S.; Miroshnichenko, L.V.; Klerkx, J.; Kovalev, S.I.; Romashkin, P.A. Chemical composition of the uranium tail storages at Kadji-Sai (southern shore of Issyk-Kul lake, Kyrgyzstan). Water Air Soil Pollut. 2004, 154, 71–83. [Google Scholar] [CrossRef]
  20. Wang, G.-Y.; Shen, Y.-P.; Qin, D.-H. Issyk-Kul Lake Level Fluctuation during 1860–2005 and Its Relation with Regional Climatic and Hydrological Changes. J. Glaciol. Geocryol. 2006, 28, 854–860. [Google Scholar]
  21. Tsigelnaya, I.D. Issyk-Kul Lake. Enclosed Seas and Large Lakes of Eastern Europe and Middle Asia; SPB Academic Publishing: Amsterdam, The Netherlands, 1995; Volume 199, p. 229. [Google Scholar]
  22. Peeters, F.; Finger, D.; Hofer, M.; Brennwald, M.; Livingstone, D.M.; Kipfer, R. Deep-water renewal in Lake Issyk-Kul driven by differential cooling. Limnol. Oceanogr. 2003, 48, 1419–1431. [Google Scholar] [CrossRef]
  23. Uulu Salamat, A.; Abuduwaili, J.; Shaidyldaeva, N. Impact of climate change on water level fluctuation of Issyk-Kul Lake. Arab. J. Geosci. 2015, 8, 5361–5371. [Google Scholar] [CrossRef]
  24. Shnitnikov, A. Water balance variability of lakes Aral, Balkhash, Issyk-Kul and Chany. In Hydrology of Lakes; Adlard & Son Ltd., Bartholomew Press: Dorking, Surrey, 1973; pp. 130–140. [Google Scholar]
  25. De Batist, M.; Imbo, Y.; Vermeesch, P.; Klerkx, J.; Giralt, S.; Delvaux, D.; Lignier, V.; Beck, C.; Kalugin, I.; Abdrakhmatov, K.E. Bathymetry and sedimentary environments of Lake Issyk-Kul, Kyrgyz Republic (Central Asia): A large, high-altitude, tectonic lake. In Lake Issyk-Kul: Its Natural Environment; Springer: Berlin, Germany, 2002; pp. 101–123. [Google Scholar]
  26. Jailoobayev, A.; Neronova, T.; Nikolayenko, A.; Mirkhashimov, I. Water Quality Standards and Norms in Kyrgyz Republic; Regional Environmental Centre for Central Asia (CAREC): Almaty, Kazakhstan, 2009. [Google Scholar]
  27. Wang, G.Y.; Shen, Y.P.; Wang, N.L.; Wu, Q.B. The Effects of Climate Change and Human Activities on the Lake Level of the Issyk-Kul during the Past 100 Years. J. Glaciol. Geocryol. 2010, 32, 1097–1105. [Google Scholar]
  28. Baetov, R. Lake Issyk-Kul. Managing Lakes and their Basins for Sustainable Future; International Lake Environment Committee Foundation: Kusatsu, Japan, 2005; pp. 193–204. [Google Scholar]
  29. Propastin, P. Assessment of climate and human induced disaster risk over shared water resources in the Balkhash Lake drainage basin. In Climate Change and Disaster Risk Management; Springer: Berlin, Germany, 2013; pp. 41–54. [Google Scholar]
  30. Vollmer, M.K.; Weiss, R.F.; Williams, R.T.; Falkner, K.K.; Qiu, X.; Ralph, E.A.; Romanovsky, V.V. Physical and chemical properties of the waters of saline lakes and their importance for deep-water renewal: Lake Issyk-Kul, Kyrgyzstan. Geochim. Cosmochim. Acta 2002, 66, 4235–4246. [Google Scholar] [CrossRef]
  31. Fereres, E.; Soriano, M.A. Deficit irrigation for reducing agricultural water use. J. Exp. Bot. 2007, 58, 147–159. [Google Scholar] [CrossRef] [PubMed]
  32. Pereira, L.S.; Oweis, T.; Zairi, A. Irrigation management under water scarcity. Agric. Water Manag. 2002, 57, 175–206. [Google Scholar] [CrossRef]
  33. Afolayan, S.O.; Ogedengbe, K.; Lateef, S.A.; Akintola, O.A.; Oladele, O.J. Response of tomato (Lycopersicium lycopersicun, CV UC82B) to drip irrigation and planting conditions. Afr. J. Agric. Res. 2014, 9, 1543–1549. [Google Scholar]
  34. Lamek Nahayo, L.L.; Zhao, X. Consideration of Precipitation Variability Under Climate Change at Kaidu River Wateshed, China. East Afr. J. Sci. Technol. 2016, 6, 16–23. [Google Scholar]
  35. Klein Tank, A.M.G.; Peterson, T.C.; Quadir, D.A.; Dorji, S.; Zou, X.; Tang, H.; Santhosh, K.; Joshi, U.R.; Jaswal, A.K.; Kolli, R.K.; et al. Changes in daily temperature and precipitation extremes in central and south Asia. J. Geophys. Res. Atmos. 2006, 111, D16. [Google Scholar] [CrossRef]
  36. Rockström, J.; Karlberg, L.; Wani, S.P.; Barron, J.; Hatibu, N.; Oweis, T.; Bruggeman, A.; Farahani, J.; Qiang, Z. Managing water in rainfed agriculture—The need for a paradigm shift. Agric. Water Manag. 2010, 97, 543–550. [Google Scholar] [CrossRef]
  37. Bouman, B.; Tuong, T.P. Field water management to save water and increase its productivity in irrigated lowland rice. Agric. Water Manag. 2001, 49, 11–30. [Google Scholar] [CrossRef]
  38. Raadgever, G.; Mostert, E.; Van de Giesen, N. Learning from collaborative research in water management practice. Water Resour. Manag. 2012, 26, 3251–3266. [Google Scholar] [CrossRef]
  39. Ward, F.A.; Pulido-Velazquez, M. Water conservation in irrigation can increase water use. Proc. Natl. Acad. Sci. USA 2008, 105, 18215–18220. [Google Scholar] [CrossRef] [PubMed]
  40. National Statistics Committee of the Kyrgzy Republic (NSCKR). Human Population of the Issyk-Kul Basin Basin Lake Region; NSCKR: Bishkek, Kyrgyzstan, 2015. [Google Scholar]
  41. Antwi-Agyei, P.; Fraser, E.D.; Dougill, A.J.; Stringer, L.C.; Simelton, E. Mapping the vulnerability of crop production to drought in Ghana using rainfall, yield and socioeconomic data. Appl. Geogr. 2012, 32, 324–334. [Google Scholar] [CrossRef]
  42. Pereira Filho, A.J.; Carbone, R.E.; Janowiak, J.E.; Arkin, P.; Joyce, R.; Hallak, R.; Ramos, C.G. Satellite Rainfall Estimates over South America-Possible Applicability to the Water Management of Large Watersheds; Wiley: Hoboken, NJ, USA, 2010. [Google Scholar]
  43. Viala, E. Water for food, water for life a comprehensive assessment of water management in agriculture. Irrig. Drain. Syst. 2008, 22, 127–129. [Google Scholar] [CrossRef]
  44. Angelakis, A.N.; Zheng, X.Y. Evolution of Water Supply, Sanitation, Wastewater, and Stormwater Technologies Globally. Water 2015, 7, 455–463. [Google Scholar] [CrossRef]
  45. Sapkota, M.; Arora, M.; Malano, H.; Moglia, M.; Sharma, A.; George, B.; Pamminger, F. An overview of hybrid water supply systems in the context of urban water management: Challenges and opportunities. Water 2014, 7, 153–174. [Google Scholar] [CrossRef]
  46. Mancosu, N.; Snyder, R.L.; Kyriakakis, G.; Spano, D. Water scarcity and future challenges for food production. Water 2015, 7, 975–992. [Google Scholar] [CrossRef]
  47. Braden, J.B.; Jolejole-Foreman, M.C.; Schneider, D.W. Humans and the water environment: The need for coordinated data collection. Water 2013, 6, 1–16. [Google Scholar] [CrossRef]
  48. Griggs, D.; Stafford-Smith, M.; Gaffney, O.; Rockström, J.; Öhman, M.C.; Shyamsundar, P.; Steffen, W.; Glaser, G.; Kanie, N.; Noble, I. Policy: Sustainable development goals for people and planet. Nature 2013, 495, 305–307. [Google Scholar] [CrossRef] [PubMed]
  49. Vonk, J.; Shackelford, T.K. The Oxford Handbook of Comparative Evolutionary Psychology; Oxford University Press: New York, NY, USA, 2012; p. 574. [Google Scholar]
  50. Libert, B.; Orolbaev, E.; Steklov, Y. Water and energy crisis in Central Asia. In China and Eurasia Forum Quarterly; Central Asia-Caucasus Institute & Silk Road Studies Program: Bishkek, Kyrgyzstan, 2008; Volume 6, pp. 9–20. [Google Scholar]
  51. Törnqvist, R.; Jarsjö, J.; Karimov, B. Health risks from large-scale water pollution: Trends in Central Asia. Environ. Int. 2011, 37, 435–442. [Google Scholar] [CrossRef] [PubMed]
Figure 1. Map of Issyk-Kul Basin Lake.
Figure 1. Map of Issyk-Kul Basin Lake.
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Figure 2. Issyk-Kul Lake water level.
Figure 2. Issyk-Kul Lake water level.
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Figure 3. Averaged annual precipitation from 1980 to 2013 precipitation as one of the lake’s water sources, can affect the water level due to its annual fluctuations.
Figure 3. Averaged annual precipitation from 1980 to 2013 precipitation as one of the lake’s water sources, can affect the water level due to its annual fluctuations.
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Figure 4. Issyk-Kul Lake Monthly Agricultural water consumption, there is gradual water demand within the months of February to July, while from July to September the demand decreases then rises again in October. This variation in agricultural water demand calls for great consideration of monthly precipitation and other water sources for the lake to be well managed under its varying demand and uses.
Figure 4. Issyk-Kul Lake Monthly Agricultural water consumption, there is gradual water demand within the months of February to July, while from July to September the demand decreases then rises again in October. This variation in agricultural water demand calls for great consideration of monthly precipitation and other water sources for the lake to be well managed under its varying demand and uses.
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Figure 5. Averaged monthly precipitation from 1980 to 2013 per station, meteorological stations reveal gradual increase of precipitation from January to April being followed by remarkable increase from May to July/August, with high marks at both the Karakol and Kyzyl-suu meteorological stations, while from September to December the intensity of precipitation decreases.
Figure 5. Averaged monthly precipitation from 1980 to 2013 per station, meteorological stations reveal gradual increase of precipitation from January to April being followed by remarkable increase from May to July/August, with high marks at both the Karakol and Kyzyl-suu meteorological stations, while from September to December the intensity of precipitation decreases.
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Table 1. Lake water consumers from 1980 to 2014.
Table 1. Lake water consumers from 1980 to 2014.
Time (Years)AgricultureManufactureHousehold
1980–19892029.4217.7427.02
1990–19999819.4618.06
2000–2014461.768.7416.55
Note: Table 1 reveals decreasing water consumption (million·m3) for all considered consumers; however, despite the reduction in water demand; agriculture is still the lake’s highest water consumer compared to manufacture and household water consumption accounts.

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Alymkulova, B.; Abuduwaili, J.; Issanova, G.; Nahayo, L. Consideration of Water Uses for Its Sustainable Management, the Case of Issyk-Kul Lake, Kyrgyzstan. Water 2016, 8, 298. https://doi.org/10.3390/w8070298

AMA Style

Alymkulova B, Abuduwaili J, Issanova G, Nahayo L. Consideration of Water Uses for Its Sustainable Management, the Case of Issyk-Kul Lake, Kyrgyzstan. Water. 2016; 8(7):298. https://doi.org/10.3390/w8070298

Chicago/Turabian Style

Alymkulova, Burul, Jilili Abuduwaili, Gulnur Issanova, and Lamek Nahayo. 2016. "Consideration of Water Uses for Its Sustainable Management, the Case of Issyk-Kul Lake, Kyrgyzstan" Water 8, no. 7: 298. https://doi.org/10.3390/w8070298

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