首页> 外文OA文献 >Annual accumulation for Greenland updated using ice core data developed during 2000-2006 and analysis of daily coastal meteorological data
【2h】

Annual accumulation for Greenland updated using ice core data developed during 2000-2006 and analysis of daily coastal meteorological data

机译:利用2000-2006年期间开发的冰芯数据和每日沿海气象数据分析,更新了格陵兰岛的年度累积量

代理获取
本网站仅为用户提供外文OA文献查询和代理获取服务,本网站没有原文。下单后我们将采用程序或人工为您竭诚获取高质量的原文,但由于OA文献来源多样且变更频繁,仍可能出现获取不到、文献不完整或与标题不符等情况,如果获取不到我们将提供退款服务。请知悉。

摘要

An updated accumulation map for Greenland is presented on the basis of 39 new ice core estimates of accumulation, 256 ice sheet estimates from ice cores and snow pits used in previous maps, and reanalysis of time series data from 20 coastal weather stations. The period 1950-2000 is better represented by the data than are earlier periods. Ice-sheetwide accumulation was estimated based on kriging. The average accumulation (95 confidence interval, or ±2 times standard error) over the Greenland ice sheet is 30.0 ± 2.4 g cm -2 a-1, with the average accumulation above 2000-m elevation being essentially the same, 29.9 ± 2.2 g cm-2 a -1. At higher elevations the new accumulation map maintains the main features shown in previous maps. However, there are five coastal areas with obvious differences: southwest, northwest, and eastern regions, where the accumulation values are 20-50 lower than previously estimated, and southeast and northeast regions, where the accumulation values are 20-50 higher than previously estimated. These differences are almost entirely due to new coastal data. The much lower accumulation in the southwest and the much higher accumulation in the southeast indicated by the current map mean that long-term mass balance in both catchments is closer to steady state than previously estimated. However, uncertainty in these areas remains high owing to strong gradients in precipitation from the coast inland. A significant and sustained precipitation measurement program will be needed to resolve this uncertainty. Copyright 2009 by the American Geophysical Union.
机译:根据39个新的冰芯累积估计,以前地图中使用的256个冰芯和冰坑估计以及对20个沿海气象站的时间序列数据的重新分析,给出了格陵兰岛的更新累积图。通过数据可以更好地代表1950-2000年期间,而不是早期时期。根据克里金法估算了整个冰盖的蓄积量。格陵兰冰盖上的平均积累量(95置信区间或标准误差的±2倍)为30.0±2.4 g cm -2 a-1,高于2000米的平均积累量基本相同,为29.9 ±2.2 g cm-2 a -1。在更高的海拔高度,新的累积图将保留以前的图所示的主要特征。但是,有五个沿海地区存在明显差异:西南,西北和东部地区的蓄积值比以前估计的低20-50;东南和东北地区的蓄积值比以前估计的高20-50 。这些差异几乎完全归因于新的沿海数据。当前地图显示的西南部较低的累积量和东南部的较高累积量意味着,两个流域的长期质量平衡比先前估计的更接近稳态。但是,由于内陆沿海地区降水的强烈梯度,这些地区的不确定性仍然很高。为了解决这种不确定性,将需要一个重要且持续的降水测量程序。美国地球物理联盟版权所有2009。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
代理获取

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