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GCM - Derived Future Climate of Arid Western India and Implications for Land Degradation

机译:GCM-印度西部干旱地区衍生的未来气候及其对土地退化的影响

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An analysis of the present and future patterns of rainfall, aridity, and wind and water erosion potentials in arid western part of Indian subcontinent, based on GCM data for A2 scenario, revealed that only few GCMs could be used with greater confidence. The study suggests strong possibility of a prolonged drought phase during 2021-2025, which may continue with some respite till the mid-century. It also shows the likelihood of aridity spreading beyond the present eastern boundary of the region duringthe same period. Since wind strength is likely to increase gradually and soils dry, the wind erosivity is expected to increase manifold across Thar Desert and Megathar region, especially from the middle of this decade, destabilizing the sandy landscape over a much larger area and contributing more to the atmospheric dust load. Likely periods of higher monsoon rainfall than the 1951-2000 mean have been identified, which may encourage higher fluvial erosion along the Aravalli foothills and Kachchh mainland due to increasing rainfall intensity that was predicted earlier by PRECIS model. Since the degradation processes are already getting accentuated by increased human pressure on the vulnerable land resources, and since there is an apprehension that normal monsoon behavior of the subcontinent has already started to get affected by the degradation processes in the region, serious efforts are needed to understand the atmosphere-land-human interaction mechanism for improving the conditions.
机译:根据A2情景的GCM数据,对印度次大陆干旱西部地区降雨,干旱以及风蚀和水蚀潜力的当前和未来模式进行的分析表明,只有少数几个GCM可以更可靠地使用。研究表明,2021-2025年干旱时期延长的可能性很大,这种情况可能会持续一段时间,直到本世纪中叶。它还显示了在同一时期内干旱扩散到该地区目前东部边界以外的可能性。由于风的强度可能会逐渐增加并且土壤变干,因此预计风侵蚀力将在塔尔沙漠和Megathar地区增加,特别是从本世纪中叶开始,这将使更大范围内的沙质景观不稳定,并进一步增加大气粉尘负荷。已经确定季风降雨量可能高于1951-2000年平均值,这可能是由于PRECIS模型较早预测的降雨强度增加,导致沿Aravalli山麓和Kachchh大陆的河流侵蚀加剧。由于人类对脆弱土地资源的压力增加已经加剧了退化过程,并且由于担心该次大陆的正常季风行为已经开始受到该区域退化过程的影响,因此需要认真努力了解改善条件的大气-地-人互动机制。

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