Estimation of Climate Change Impacts on Water Balance in the Aral Sea Basin using Terrestrial Water Circulation Model

  • TOUGE Yoshiya
    京都大学 防災研究所気象・水象災害研究部門
  • TANAKA Kenji
    京都大学 防災研究所水資源環境研究センター
  • NAKAKITA Eiichi
    京都大学 防災研究所気象・水象災害研究部門

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Other Title
  • アラル海流域における陸域水循環モデルを用いた気候変動の水需給バランスへの影響評価
  • アラル カイリュウイキ ニ オケル リクイキスイ ジュンカン モデル オ モチイタ キコウ ヘンドウ ノ ミズ ジュキュウ バランス エ ノ エイキョウ ヒョウカ

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Abstract

 In the Aral Sea Basin, serious drought was induced by huge-scale irrigation projects. Toward sustaineble water management, impacts of climate change on water resource and water demand should be quantitatively estimated to provide a scientific basic information for the rational planning.<br> In this study, terrestrial water circulation model was applied to project future water resource and demand. It is mainly consist of land surface model SiBUC (Simple Biosphere including Urban Canopy). In its irrigation scheme, local irrigation rule was reflected through in situ measurement on testing farms in Uzbekistan and furrow irrigation can be considered which is generally selected in this basin. The meteorological data for the model input are from Meteorological Research Institute atmospheric general circulation model (MRI-AGCM3.2S) based on A1B scenario. Spatial resolution is about 20km and time resolution is one hour. Since the GCM projected that both temperature and precipitation will increase in the whole basin, future drought situation should be quantitatively analyzed by physical model.<br> As a result of the analysis, water resource will not change since increment of precipitation will consumed by evapotranspiration increase and little water will additionally flow out as surface runoff. On the other hand, water demand will increase due to temperature rise especially in the arid region. In the limitted area in mountainous region, precipitation increase reduces water demand for irrigation. Comprehensively, drought situation in this basin will increase under the future climate.

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