the support from the Office of Polar Programs,National Science Foundation(Grant Nos.1924730,1951720,1951603,and 2205398),which is greatly appreciated.
The 18th Workshop on Antarctic Meteorology and Climate was held on 31 May through 2 June 2023.The Antarctic Meteorological Research and Data Center hosted this hybrid workshop at the Pyle Center at the University of W...
support from the US National Science Foundation(Grant Nos.1924730,2301362,and 2205398).
Extreme cold temperatures were observed in July and August 2023,coinciding with the WINFLY(winter fly-in)period of mid to late August into September 2023,meaning aircraft operations into McMurdo Station and Phoenix Ai...
supported by the National Key Research and Development Program of China(Grant No.2022YFE0106300);the National Natural Science Foundation of China(Grant Nos.42105072,41941009,41922044);the Guangdong Basic and Applied Basic Research Foundation(Grant Nos.2021A1515012209,2020B1515020025);the China Postdoctoral Science Foundation(Grant Nos.2021M693585);the Norges Forskningsråd(Grant No.328886).
It is crucial to appropriately determine turbulent fluxes in numerical models.Using data collected in East Antarctica from 8 April to 26 November 2016,this study evaluates parameterization schemes for turbulent fluxes...
supported by the National Natural Science Foundation of China (Grant Nos.41941010,41771064 and 41776195);the National Basic Research Program of China (Grant No.2016YFC1400303);the Basic Fund of the Chinese Academy of Meteorological Sciences (Grant No.2018Z001)。
Long-term,ground-based daily global solar radiation (DGSR) at Zhongshan Station in Antarctica can quantitatively reveal the basic characteristics of Earth’s surface radiation balance and validate satellite data for t...
the financial support to CESAM (UID/AMB/ 50017/2019) through national funds and FCT grant CIRCNA/CAC/ 0273/2019;National Institute of Polar Research (NIPR) Project Research No. KP302
Atmospheric rivers(ARs)are an important component of the hydrological cycle linking moisture sources in lower latitudes to the Antarctic surface mass balance.We investigate AR signatures in the atmospheric vertical pr...
the Brazilian Antarctic Program(PROANTAR);was financed with funds from the Brazilian National Council for Scientific and Technological Development(CNPq)Split Fellowship Program(Grant No.200386/2018-2);from the CNPq projects 465680/2014-3 and 442761/2018-0.We thank the Centro Polar e Climático(CPC/UFRGS);the Department of Geological Sciences(CWU)faculty and staff for their support of this work.
This work presents the refractory black carbon(rBC)results of a snow and firn core drilled in West Antarctica(79°55'34.6"S,94°21'13.3"W)during the 2014?15 austral summer,collected by Brazilian researchers as part of...
supported by the National Natural Science Foundation of China(Grant Nos.41006115 and 41376005);the Chinese Polar Environmental Comprehensive Investigation and Assessment Program;the Chinese National Key Basic Research Project(2011CB309704)
The snow/sea-ice albedo was measured over coastal landfast sea ice in Prydz Bay, East Antarctica(off Zhongshan Station)during the austral spring and summer of 2010 and 2011. The variation of the observed albedo was ...
supported by the project "Investigation of Climate Change Mechanisms by Observation and Simulation of the Polar Climate Past and Present" (PE14010) of the Korea Polar Research Institute;the National Natural Science Foundation of China (Grant No.41375003);the Beijing High Education Young Elite Teacher Project and the Chinese Academy of Sciences (Grant No.XDA05110303)
Two parallel sets of numerical experiments (an ozone-hole simulation and a non-ozone-hole simulation) were performed to investigate the effect of ozone depletion on surface temperature change using the second spectr...
funded by the National Natural Science Foundation of China under Grant No.40905048;the German Bosch Foundation,and the program of basic research and operating of CAMS
Climate and forecast mode simulations with the regional climate model HIRlam-ECHAM(HIRHAM) are evaluated over a pan-Antarctic domain. The ability of the model to simulate temperature and wind profiles in the troposp...
This research was partially funded by the Chinese Polar Program Strategic Research Fund (No. 20080218);the National Natural Science Foundation of China (40233032-40640420556);MOST(2006BAB18B03 and 2006BAB18B05)
The European Center for Medium-Range Weather Forecast (ECMWF) Re-Analysis (ERA-40) and the National Centers for Environmental Prediction-National Center for Atmospheric Research (NCEP-NCAR) ECMWF (ERA-40) and ...