supported by the National Natural Science Foundation of China(Grant Nos.41876230&41376192);the National Basic Research Program of China(Grant No.2013CBA01804);the Chinese Polar Environment Comprehensive Investigation&Assessment Programs(Grant No.CHINARE2017-04-01)
The ages and accumulation rates of ice are important boundary conditions for paleoclimatic ice models. Radardetected isochronic layers can be used to date the ice column beneath the ice surface and infer past accumula...
supported by the National Key Basic Research Program of China(Grant No.2013CBA01804);the National Science Foundation of China(Grant Nos.41425003 and 41401079);the State Oceanic Administration of the People’s Republic of China Project on Climate in Polar Regions(Grant No.CHINARE2016-2020);the Key Research Program of the Chinese Academy of Sciences(Grant No.KJZD-EW-G03);the Opening Founding of the State Key Laboratory of Cryospheric Sciences(Grant No.SKLCS-OP-2016-03)
Changes in the form of precipitation have a considerable impact on the Arctic cryosphere and ecological system by influencing the energy balance and surface runoff. In this study, station observations and ERA-Interim ...
supported by grants from the Hundred Talents Program of the Chinese Academy of Sciences,the Science Fund for Creative Research Groups of the National Natural Science Foundation of China(NSFC)(41425003,41121001);the Ministry of Science and Technology of China(Mo ST,2013CBA01804);the Scientific Research Foundation of the Key Laboratory of Cryospheric Sciences(SKLCS-ZZ-2017-01)
Dissolved organic matter(DOM) is an important component of ice cores but is currently poorly characterized. DOM from one Holocene sample(HS, aged at 1600–4500 B.P.) and one Last Glacial Maximum sample(LS, aged at 21...
supported by the Ministry of Science and Technology of China(MOST, 2013CBA01804);the National Nature Science Foundation of China (41425003,41401079, 41476164 and 41625014);the key project of CAMS:Research on the Key Processes of Cryospheric Rapid Changes (KJZD-EW-G03);the Opening Founding of State Key Laboratory of Cryospheric Sciences(SKLCSOP-2016-03);the State Key Laboratory of Cryospheric Sciences (SKLCS-ZZ-2017)
Based on the field measurements in Barrow, Alaska within the period of April-May 2015, we investigate the sources and variations of elemental carbon(EC) and organic carbon(OC) in the surface layer of snowpack on sea i...
funded by the National Key Basic Research Program of China (Grant No.2013CBA01804);the Natural Science Foundation of China (Grant Nos.41206175 and 41576182);the Scientific Research Foundation for the Introduction of Talent by Shandong Normal University
Recent snow height measurements(2008–15) from nine automatic weather stations(AWSs) on the Ross Ice Shelf are used to examine the synoptic and seasonal variability in snow accumulation,and also to evaluate the perfor...
supported by the National Basic Research Program of China(Grant No. 2013CBA01804);the National Natural Science Foundation of China(Grant Nos.41425003 & 41601070);the State Oceanic Administration of the People s Republic of China Project on Climate in Polar Regions(Grant No. CHINARE2016-2020);Climate Change Estimation Program by China Meteorological Administration(Grant No.CCSF201332)
A high-frequency and precise ultrasonic sounder was used to monitor precipitated/deposited and drift snow events over a 3-year period(17 January 2005 to 4 January 2008) at the Eagle automatic weather station site,inla...
funded by the Ministry of Science and Technology of China (2013CBA01804);the National Nature Science Foundation of China (41425003, Y51101P1A1);the key project of CAMS: Research on the key processes of Cryospheric rapid changes (KJZD-EW-G03-04);the Opening Founding of State Key Laboratory of Cryospheric Sciences (SKLCS-OP-2016-03)
This paper gives an overview of the current understanding of the observations of black carbon(BC) in snow and ice, and the estimates of BC deposition and its radiative forcing over the Arctic. Both of the observations...