干旱区研究 ›› 2021, Vol. 38 ›› Issue (6): 1514-1523.doi: 10.13866/j.azr.2021.06.03
王振1,2(),李均力1,3(),包安明1,3,张久丹1,2,白洁1,3
收稿日期:
2021-03-28
修回日期:
2021-07-17
出版日期:
2021-11-15
发布日期:
2021-11-29
通讯作者:
李均力
作者简介:
王振(1995-),男,硕士研究生,主要从事干旱区水资源与湖泊变化机理研究. E-mail: 基金资助:
WANG Zhen1,2(),LI Junli1,3(),BAO Anming1,3,ZHANG Jiudan1,2,BAI Jie1,3
Received:
2021-03-28
Revised:
2021-07-17
Online:
2021-11-15
Published:
2021-11-29
Contact:
Junli LI
摘要:
巴里坤湖是天山东部山间内陆封闭型湖泊,了解巴里坤湖的演变特征对于开展湖泊保护与生态环境治理具有重要意义。利用308景Landsat系列和Sentinel 2遥感影像提取1995—2020年湖泊水面的时间序列,并结合巴里坤气象站资料以及从遥感影像上提取的耕地面积数据,分析湖泊在气候变化与人类活动影响下的变化趋势。结果表明:湖泊变化经历了2个阶段:1995—2006年萎缩,从年均值57.33 km2下降到35.53 km2,下降速率1.98 km2·a-1,萎缩35.79%;2006—2020年扩张,从年均值35.53 km2上升到46.59 km2,上升速率0.79 km2·a-1,扩张31.12%。多年湖泊面积的月变化统计表明:湖泊在5月达到最大值(73.09±21.01)km2,11月达到最小值(43.90±16.97)km2。影响因素:1995—2006年,降水变化幅度较小,农业用水与蒸发量增加是巴里坤湖萎缩的主要原因;2006年后,巴里坤县出台多种湿地保护措施,耕地面积扩张趋势得到控制,降水显著增加与蒸发量减少成为湖泊面积扩张的主要原因。
王振,李均力,包安明,张久丹,白洁. 1995—2020年新疆巴里坤湖面积时序变化及归因[J]. 干旱区研究, 2021, 38(6): 1514-1523.
WANG Zhen,LI Junli,BAO Anming,ZHANG Jiudan,BAI Jie. Temporal variation in the Barkol Lake area and its driving factors in 1995-2020[J]. Arid Zone Research, 2021, 38(6): 1514-1523.
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