Climate Change Impact to the River Runoff: Regional Study for the Central Asian Region NATALYA AGALTSEVA Research Hydrometeorological institute (NIGMI) Uzbekistan

1.Climate change in Uzbekistan 2.The approach to the assessment of climate changes impact on the rivers runoff on the base of climatic scenarios: problems and solutions 3.Climate change impact on water resources of Aral See Basin 3. The water resources monitoring Basic problems

Data of monitoring show: There is a tendency to increasing of the air temperature and changes of cold and hot year seasons lengths for Central Asia territory; Climate dryness becomes more severe ; 2004 year was the warmest during all period of observation There are significant variations of precipitation under their slow tendency to increasing. The complicated reaction of runoff forming zone and runoff dissemination zone to the recent climate changes and anthropogenic impacts takes place. Climate change in Uzbekistan

Grid points SCENGEN and reference stations of Uzbekistan. Climate scenario design for Uzbekistan Metodology IPCC : Application of MAGICC: selection of the emission scenarios from IPCC SRES storylines Application of SCENGEN: analysis of models uncertainty over the region and selection of the appropriate GCMs Application of statistical downscaling method: Creation of archive in grid points based on observation data (area averaged anomalies are considered as best forecasts of selected GCM). Construction of regression equations between data in grid points and station data.

For construction of regional climate scenarios it is necessary to use GHG (greenhouse gases) scenarios. А1(A1B,A1T,A1FI), А2, В1, В2 GHG scenarios are describing various variants of social and economic development. А1, А2 – the scenarios describing a situation, when preference to global priorities, В1, В2 – regional B1. The emphasis is on global solutions to economic, social and environmental sustainability. Climate scenario design for Uzbekistan

Rise in temperature °С Change of precipitation, % from norm Для оценки ожидаемых изменений месячных температур воздуха и осадков были выбраны шесть GCM моделей Six GCM models had been chosen for an estimation of expected changes of monthly air temperatures and precipitation Вывод: Усреднение ряда моделей позволяет уменьшить неопределенность сценариев Conclusion: Averaging of outputs by a few models allows to reduce uncertainty of scenarios Climate scenario design for Uzbekistan

Выводы Для проведения оценки воздействия изменения климата в Узбекистане предлагается использовать региональные климатические сценарии, построенные в соответствии со сценариями эмиссии А2 (неблагоприятный ) и В2 (умеренный). На ближнесрочную (2030) и среднесрочную (2050) перспективы различия в ожидаемых изменениях температуры будут невелики, а к 2080 году возрастут. Conclusions It is supposed to use the regional climate scenarios are based upon emission scenarios A2 (unfavorable) and B2 (moderate) to assess climate changes in Uzbekistan. The air temperature changes will be insignificant for short-term (2030) and middle-short (2050) perspectives but go up by The expected air temperature changes by A2, B2 scenarios for Uzbekistan A2 B2 by 2030 about by 2050 about by 2080 about

The river flow is concentrated in the two largest transboundary rivers: the Amudarya (78.5 km3 per year) and Syrdarya River (37.1 km3 per year), which run down from the mountains to the plains, cross the deserts and flow into the Aral Sea Sustainable development needs to have the rational use of the limited fresh water resources

SNOW COVER FORMATION Glacial contribution Transformation of contributions to runoff Melting water and rain contribution The degree of the impact the expected climate changes to the river run-off in region can be assessed with help of the mathematical models of run-off forming SET OF THE MODELS Methodical approach to the assessment of climate changes impact to the rivers runoff

System AISHF An automated information system of runoff formation has been developed for practical application of the mathematical models of runoff formation

The complicated reaction of runoff forming zone and runoff dissemination zone to the recent climate changes and anthropogenic impacts takes place. Sources of the mountain rivers feeding: a seasonal snow cover melting, historical accumulation of ice and firn in the glaciers, rains are very sensitive to change of climatic parameters Seasonal snow plays a key role in the feeding of the rivers in the Aral sea basin. Some reduction snow supplies in the basins most of all rivers is observed Climate change impact on water resources of Aral See Basin

Glaciological observations were run in the runoff formation zones since The glaciological observations were practically stopped during last years. During 1957 – 1980 the Pamir-Alay glaciers lost 113 km3 (19%) of their water supplies. The lost raised up to 14% more of supplies by Glaciers lost will be increased to 10% more of the initial supplies by Glaciers are the single source of pure water in Central Asia CHANGES OF THE PAMIR-ALAY GLACIATION EXTENT IN THE 2nd PART OF XX CENTURY

km 2 ? ? ? ? Reduction of the glacier area in the separate river basins During the Abramov glacier lost 21 meter of water layer and it amounts 18% of its mass. By 2020 году loss of 17% of its ice is expected Currently only the separate glacial areas are estimated on the base of satellite information Balance of the Abramov glacier mass in 1977 (-161 cm)

Для сценария А2 к 2030 году а бассейнах Амударьи и Сырдарьи существенных изменений водных ресурсов не ожидается. The significant water resources` changes are not expected by 2030 per A2 scenario. К 2050 году возможно сокращение водных ресурсов по бассейну реки Амударьи на %. По бассейну реки Сырдарьи возможно сокращение на 2-5%. Water resources decrease up to 10-15% for Amudarya and up to 2-5% for Syrdarya by 2050 is expected Climate change impact on water resources of Aral See Basin

2030 норма Climate change impact on water resources of Aral See Basin Our preliminary calculations have shown: There is tendency to decreasing of the snow supplies; Glaciers continue to be reduced with rates of 0,2 % - 1 % one year; Increase of the evaporation in river basins; Growth in the variability of the precipitation and intensification of all factors for the years with drought With the further increase of air temperatures the river runoff decreases. Rivers of Amu Darya river basin and small rivers are more sensitive to warming climate It is expected that runoff variability of all basins will go up.

Выводы: Таким образом, ни один из рассмотренных климатических сценариев, отражающих «потепление климата», не предполагает увеличения располагаемых водных ресурсов. Ожидаемое повышение испаряемости в условиях потепления увеличит потери воды в зонах орошения, что потребует дополнительных затрат воды. При существующей в настоящее время ситуации в орошаемом земледелии, изменение климата неизбежно приведет к усилению водного дефицита Conclusion: Thus, none of the considered climatic scenarios of « warming of a climate », does not assume increase in available water resources. Expected increase of evaporation under conditions of climate warming will increase losses of water in the irrigated areas that will increase water demand there. Climate change will increase of water deficit for irrigation needs under current situation in irrigation. Climate change impact on water resources of Aral See Basin

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