首页> 外文期刊>Geophysical Research Letters >Initial in situ measurements of perennial meltwater storage in the Greenland firn aquifer
【24h】

Initial in situ measurements of perennial meltwater storage in the Greenland firn aquifer

机译:格陵兰杉木含水层中多年生融水储量的初始原位测量

获取原文
获取原文并翻译 | 示例
           

摘要

[1] A perennial storage of water in a firn aquifer was discovered in southeast Greenland in 2011. We present the first in situ measurements of the aquifer, including densities and temperatures. Water was present at depths between ~12 and 37m and amounted to 18.7 ± 0.9 kg in the extracted core. The water filled the firn to capacity at ~35m. Measurements show the aquifer temperature remained at the melting point, representing a large heat reservoir within the firn. Using model results of liquid water extent and aquifer surface depth from radar measurements, we extend our in situ measurements to the Greenland ice sheet. The estimated water volume is 140 ± 20 Gt, representing ~0.4mm of sea level rise (SLR). It is unknown if the aquifer temporary buffers SLR or contributes to SLR through drainage and/or ice dynamics.
机译:[1] 2011年在格陵兰岛东南部发现了一种烧成含水层中的多年生水。我们介绍了该含水层的第一个原位测量值,包括密度和温度。水存在的深度在〜12至37m之间,在提取的岩心中达18.7±0.9 kg。水注入鱼缸至约35m。测量表明,含水层温度保持在熔点,表示炉膛内有大量储热器。利用来自雷达测量的液态水范围和含水层表面深度的模型结果,我们将原位测量扩展到格陵兰冰盖。估计的水量为140±20 Gt,代表海平面上升(SLR)约0.4mm。尚不清楚含水层是临时缓冲SLR还是通过排水和/或冰动力学对SLR起作用。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号