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基于PlanetScope影像的格陵兰冰面融水监测

朱雨欣 张闻松 杨康

极地研究2023,Vol.35Issue(4):508-516,9.
极地研究2023,Vol.35Issue(4):508-516,9.DOI:10.13679/j.jdyj.20220419

基于PlanetScope影像的格陵兰冰面融水监测

Surface meltwater on the Greenland ice sheet mapped from PlanetScope small satellite imagery

朱雨欣 1张闻松 1杨康2

作者信息

  • 1. 南京大学地理与海洋科学学院,江苏 南京 210023
  • 2. 南京大学地理与海洋科学学院,江苏 南京 210023||江苏省地理信息技术重点实验室,江苏 南京 210023||南方海洋科学与工程广东省实验室(珠海),广东 珠海 519080
  • 折叠

摘要

Abstract

Surface melt of the Greenland ice sheet and its impact on rising sea levels have become hot topics in international research.Each summer,surface meltwater forms on the Greenland ice sheet,forming supragla-cial lakes,supraglacial rivers,and water-filled crevasses.There is a large area of surface meltwater,which exhibits complex structure,and changes rapidly over time.Regional climate models do not accurately simu-late the distribution of surface meltwater,and medium resolution satellite images may not reflect spatial and temporal changes in surface meltwater.CubeSats,such as PlanetScope,allow dynamic monitoring of surface meltwater by providing near-daily satellite observation at 3 m spatial resolution.In this study,we extracted surface meltwater in a typical internally drained catchment in the southwest Greenland ice sheet using Plan-etScope images.We then constructed a formula to estimate meltwater depth from the PlanetScope images and compared meltwater volume estimated by satellite images and meltwater runoff simulated by the MAR v3.11 model.The results showed that the open water fraction(OWF)of surface meltwater in the catchment first rose then decreased during July and August 2019,peaking on 12 July(8.7%).The surface meltwater depth in the catchment ranged from 0.2 to 1.5 m,and the supraglacial lakes were the deepest(0.9 m±0.2 m),followed by the mainstem of supraglacial rivers(0.6 m±0.1 m),and the tributaries of supraglacial rivers(0.5 m±0.1 m).The OWF,meltwater volume and daily runoff simulated by MAR were positively correlated,indicating that meltwater runoff directly supplies supraglacial lakes and rivers.The surface meltwater stor-age capacity is limited(<1%),and the catchment is efficiently transporting meltwater into the ice sheet.

关键词

冰面融水/PlanetScope/遥感观测/区域气候模型/格陵兰冰盖

Key words

surface meltwater/PlanetScope/remote sensing observation/regional climate model/Greenland ice sheet

引用本文复制引用

朱雨欣,张闻松,杨康..基于PlanetScope影像的格陵兰冰面融水监测[J].极地研究,2023,35(4):508-516,9.

基金项目

国家自然科学基金(41871327)和中国科学院战略性先导科技专项(XDA19070201)资助 (41871327)

极地研究

OA北大核心CSCDCSTPCD

1007-7073

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