Field activities of the "Snow Impurity and Glacial Microbe effects on abrupt warming in the Arctic" (SIGMA) Project in Greenland in 2011-2013(2011-2013年グリーンランドにおけるSIGMAプロジェクトの野外活動報告)

IF 1 Q4 GEOGRAPHY, PHYSICAL
T. Aoki, S. Matoba, J. Uetake, Nozomu Takeuchi, Hideaki Motoyama
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引用次数: 39

Abstract

Field activities of the “Snow Impurity and Glacial Microbe effects on abrupt warming in the Arctic” (SIGMA) Project in Greenland in the summer season of 2011-2013 are reported; this consists of (1) glaciological and meteorological observations and (2) biological observations. In 2011, we conducted a field reconnaissance in the Qaanaaq, Ilulissat and Kangerlussuaq areas to enable continuous meteorological observations with automatic weather stations (AWS), campaign observations for glaciology, meteorology and Biology and shallow ice core drilling, which were planned for 2012-2014. Based on the results, we chose the Qaanaaq area in northwest Greenland as our main activity area and the Kangerlussuaq area in mid-west Greenland partly for biological observations. In 2012, we conducted field observations for (1) and (2) mentioned above together with installations of two AWSs at site SIGMA-A on The Greenland ice sheet (GrIS) and at site SIGMA-B on the Qaanaaq ice cap (QIC) from June to August. Surface snow and ice over all of the QIC melted in July and August 2012, and most of the Glacier surface appeared to be dark-colored, probably due to mineral dust and glacial microbial products. In 2013, we carried out similar observations in the Qaanaaq area. However, the weather and Glacier surface conditions were considerably different from those in 2012. Snow cover over the summer of 2013 remained over large areas with elevations higher than about 700 m on QIC. Biological activity on the Glacier surface appears to be substantially lower as compared to that in 2012.
Field activities of the "Snow Impurity and Glacial Microbe effects on abrupt warming in the Arctic"SIGMA计划2011-2013 (SIGMA计划2011-2013年格陵兰野外活动报告)
报道了2011-2013年夏季格陵兰岛“雪杂质和冰川微生物对北极突变增温的影响”(SIGMA)项目的野外活动;这包括(1)冰川学和气象观测和(2)生物观测。2011年,我们在Qaanaaq、Ilulissat和Kangerlussuaq地区进行了野外侦察,以实现自动气象站(AWS)的连续气象观测、冰川学、气象学和生物学的运动观测和浅层冰芯钻探,计划于2012-2014年进行。在此基础上,我们选择了格陵兰西北部的Qaanaaq地区作为我们的主要活动区,并选择了格陵兰中西部的Kangerlussuaq地区进行部分生物观测。2012年6 - 8月,我们对上述(1)和(2)进行了野外观测,并在格陵兰冰盖(GrIS)的SIGMA-A站点和Qaanaaq冰盖(QIC)的SIGMA-B站点安装了两台AWSs。2012年7月和8月,QIC上的冰雪全部融化,大部分冰川表面呈现深色,可能是矿物粉尘和冰川微生物产物造成的。2013年,我们在卡纳克地区进行了类似的观测。然而,天气和冰川表面条件与2012年有很大不同。2013年夏季,QIC上海拔700 m以上的大片地区仍有积雪。与2012年相比,冰川表面的生物活动似乎大大降低。
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来源期刊
Bulletin of glaciological research
Bulletin of glaciological research GEOGRAPHY, PHYSICAL-
CiteScore
2.20
自引率
20.00%
发文量
1
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