Variasi Regim Lengas dan Suhu Tanah Pada Lahan yang Mengalami Penutupan Awan Rendah Berbasis Peta Terra Modis di Pulau Lombok

Reni Anggraeni, Mahrup Mahrup, I. Kusnarta, Putu Silawibawa
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引用次数: 1

Abstract

Soil moisture and temperature are parameters of soil physical properties that are closely related to climatic variations. Descriptive Research on "Variation of Moisture Regime and Soil Temperature on Land with Low Cloud Cover" has been done, to determine the variation of soil moisture and soil temperature on land with permanently low cloud cover based on the Terra Modis map on the island of Lombok. Low cloud cover data was obtained from Terra Modis satellite data which were delineated by Lombok maps. Daily rainfall data were collected from the Climatology Meteorology and Geophysics Agency (BMKG) Kediri Station. Moisture and soil temperature were measured periodically at 10 day intervals, for two consecutive months (March and April, 2020). The results showed that soil moisture varied temporally. Soil moisture content was higher in areas with low cloud cover in the dryland with soils type of Typic Eutrudept, Inceptisols order, than in areas without cloud permanent cover. Soil temperature in the open zone (without low cloud cover) was higher than in the zone that always experiences closure
龙目岛陆地地温的变化和土壤温度的变化,使龙目岛地面上的低云逐渐消失
土壤湿度和温度是土壤物理性质的参数,与气候变化密切相关。以龙目岛Terra Modis地图为基础,对“低云量条件下陆地上的湿度状况和土壤温度变化”进行了描述性研究,确定了长期低云量条件下陆地上的土壤湿度和温度变化。低云量数据来自Terra Modis卫星数据,由龙目岛地图圈定。日降雨量数据收集自气候气象学和地球物理局(BMKG) Kediri站。连续2个月(2020年3月和4月),每隔10天定期测量水分和土壤温度。结果表明,土壤水分具有时间变化特征。土壤类型为typyeutrdept, ineptisols目的旱地低云量区土壤含水量高于无云永久覆盖区。开放区(无低云量)土壤温度高于封闭区
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