Climate Change, Regional Water Balance and Land Use Policy, in the Watershed of Lake Kinneret (Israel)

M. Gophen, M. Meron, Valerie Levin-Orlov, Y. Tsipris, Mordechay Peres
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引用次数: 6

Abstract

Long term data record (1944-2018) of climatological conditions in the Lake Kinneret and its watershed ecosystems was statistically evaluated and the impact of Anthropogenic operations was included as well. Precipitation input source is obviously uncontrolled natural component whilst the other three regional water outflows pathways are under anthropogenic control: Evapo-transpiration (ET), Runoff and underground flows. Indications for climate change expressed as air warming with consequences on regional (watershed and the lake) water resources and consumption capacities policy in the drainage basin and in the Lake are discussed. The decline of air temperature from 1940 to 1970s is probably due to a change in the Albedo effect. After the decline air temperature was twisted towards elevation. Climate change caused a decline in rainfall, followed by a reduction of Jordan and other river discharges and underground flows, accompanied by a decline of WL. With respect to climate change, water allocation for agricultural consumption was shrunk.
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气候变化、区域水平衡与土地利用政策——以以色列Kinneret湖流域为例
对金纳雷特湖及其流域生态系统气候条件的长期数据记录(1944-2018年)进行了统计评估,并纳入了人为活动的影响。降水输入源是明显不受控制的自然成分,而蒸散发、径流和地下流是受人为控制的3个区域水流出途径。气候变化的迹象表现为空气变暖对区域(流域和湖泊)水资源的影响以及流域和湖泊的消费能力政策。从1940年到1970年的气温下降可能是由于反照率效应的变化。在下降之后,气温向高处扭曲。气候变化导致降雨量减少,随后约旦河等河流流量和地下流量减少,WL下降。在气候变化方面,农业用水分配减少。
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