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Analysis of climate change impacts on lake ice phenology in Canada using the historical satellite data record

机译:利用历史卫星数据记录分析气候变化对加拿大湖泊冰物候的影响

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摘要

Variability and trends in lake ice dynamics (i.e. lake ice phenology) are related to climate conditions. Climate influences the timing of lake ice melt and freeze onset, ice duration, and lake thermal dynamics that feedback to the climate system initiating further change. Phenology records acquired in a consistent manner and over long time periods are required to better understand variability and change in climate conditions and how changes impact lake processes. In this study, we present a new technique for extracting lake ice phenology events from historical satellite records acquired by the series of Advanced Very High Resolution Radiometer (AVHRR) sensors. The technique was used to extend existing in-situ measurements for 36 Canadian lakes and to develop records for 6 lakes in Canada's far north. Comparison of phenology events obtained from the AVHRR record and in-situ measurements show strong agreement (20 lakes, 180 cases) suggesting, with high confidence especially in the case of break-up dates, the use of these data as a complement to ground observations. Trend analysis performed using the combined in-situ and AVHRR record similar to 1950-2004 shows earlier break-up (average - 0.18 days/year) and later freeze-up (average 0.12 days/year) for the majority of lakes analyzed. Less confidence is given to freeze-up date results due to lower sun elevation during this period making extraction more difficult. Trends for the 20 year record in the far north showed earlier break-up (average 0.99 days/year) and later freeze-up (average 0.76 days/year). The established lake ice phenology database from the historical AVHRR image archive for the period from 1985 to 2004 will to a certain degree fill data gaps in the Canadian in-situ observation network. Furthermore, the presented extraction procedure is not sensor specific and will enable continual data update using all available satellite data provided from sensors such as NOAA/AVHRR, MetOp/AVHRR, MODIS, MERIS and SPOT/VGT. Crown Copyright (c) 2006 Published by Elsevier Inc. All rights reserved.
机译:湖冰动力学的变化和趋势(即湖冰物候)与气候条件有关。气候会影响湖泊冰融化和冻结开始的时间,冰的持续时间以及湖泊热动力学,这些反馈到气候系统,从而引发进一步的变化。需要以长期一致的方式获得的物候记录,以更好地了解气候条件的多变性和变化以及变化如何影响湖泊过程。在这项研究中,我们提出了一种新技术,该技术用于从由一系列非常甚高分辨率辐射计(AVHRR)传感器获取的历史卫星记录中提取湖冰物候事件。该技术被用于扩展加拿大36个湖泊的现有实地测量,并开发了加拿大最北部6个湖泊的记录。从AVHRR记录和现场测量获得的物候事件的比较显示出强烈的一致性(20个湖泊,180例),这表明,尤其是在破裂日期的情况下,具有很高的置信度,这些数据被用作地面观测的补充。使用与1950-2004年相似的现场和AVHRR组合记录进行的趋势分析显示,对于所分析的大多数湖泊而言,分解的时间更早(平均-0.18天/年),随后的分解时间(平均0.12天/年)。由于在此期间较低的太阳高度,因此对冻结日期的结果信心不足,这使得提取更加困难。远北地区20年记录的趋势显示,中断时间较早(平均0.99天/年),冻结时间较晚(平均0.76天/年)。 1985年至2004年期间从历史AVHRR图像档案库建立的湖泊冰物候数据库将在一定程度上填补加拿大原位观测网络中的数据空白。此外,提出的提取程序不是特定于传感器的,并且将使用从传感器提供的所有可用卫星数据(例如NOAA / AVHRR,MetOp / AVHRR,MODIS,MERIS和SPOT / VGT)进行连续数据更新。 Crown版权所有(c)2006,由Elsevier Inc.发行。保留所有权利。

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