海南島蒸發量的變化特征及其影響因子分析
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海南省氣象局青年基金項目(HNQXQN201703)資助


Variation of Pan Evaporation over Hainan Island and Its Influence Factors
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    摘要:

    利用海南島18個氣象觀測站1966—2001年逐日20 cm口徑小型蒸發皿蒸發量及氣象要素資料,通過數理統計方法分析了海南島年和四季的蒸發量變化特征及氣象因子對蒸發量的影響。結果表明:從時間上看,海南島年蒸發量變化呈波動式下降,蒸發量的減少主要出現在春季,冬季和夏季次之。從空間上看,年蒸發量呈東北少、西南多的分布,其大值區主要集中在西南部,小值區主要集中在東北部和中部地區。MK檢驗說明年與春冬兩季蒸發量的變化呈下降趨勢且在1994年前后發生突變。影響蒸發量變化的因子中,日照時數和風速是造成蒸發量減小的主要因子,降水量的影響僅次于風速和日照時數,而氣溫不是造成海南島蒸發量減小的主要因子,相對濕度可能是海南島的蒸發量減小的影響因子。

    Abstract:

    Based on the daily data of 20cm evaporating pans as well as other meteorological factors of 18 automatic meteorological observation stations from 1966 to 2001 over Hainan Island, changes in pan evaporation and their causes are analyzed by the methods of ArcGIS and the mathematical statistics. The results show that the annual evaporation of Hainan Island showed a fluctuating decline, and the decrease of annual evaporation mainly occurred in spring, winter and summer. The annual evaporation was less in the northeast and greater in the southwest. The large value areas were mainly concentrated in the southwest, while the smaller ones were mainly concentrated in the northeast and middle areas. The MK test confirms that annual evaporation had significantly decreasing trends and the significant mutation year was about 1994. Among the change factors affecting evaporation, the sunshine duration and wind speed were the main factors that caused the decrease of evaporation. The influence of precipitation on the evaporation of Hainan Island was second only to the wind speed and sunshine hours. The temperature was not the main factor for decreasing evaporation, and humidity might be the influence factor of the of Hainan Island decreasing evaporation.

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施晨曉,羊清雯,王小潔,程洪濤,鄭虹暉.海南島蒸發量的變化特征及其影響因子分析[J].氣象科技,2019,47(3):439~449

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  • 收稿日期:2018-05-23
  • 定稿日期:2019-01-22
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  • 在線發布日期: 2019-06-25
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