DOI: 10.25923/hcm7-az41 J. E. Walsh1,2, S. Bigalke3, S. A. McAfee4, R. Lader2, M. C. Serreze5, and T. J. Ballinger2 1Alaska Center for Climate Assessment and Policy, University of Alaska Fairbanks, Fairbanks, AK, USA 2International Arctic Research Center, University of Alaska Fairbanks, Fairbanks, AK, USA 3Department of Geography, Portland State University, Portland, OR, USA 4Department of […]
DOI: 10.25923/yetx-rs76 K. Poinar1, K. D. Mankoff2,3, R. S. Fausto4, X. Fettweis5, B. D. Loomis6, A. Wehrlé7, C. D. Jensen8, M. Tedesco9, J. E. Box4, and T. L. Mote10 1University at Buffalo, Buffalo, NY, USA 2Goddard Institute of Space Studies, NASA, New York, NY, USA 3Autonomic Integra, New York, NY, USA 4Geological Survey of Denmark
Greenland Ice Sheet Read More »
DOI: 10.25923/f5t4-b865 W. N. Meier1, A. Petty2, S. Hendricks3, L. Kaleschke3, D. Divine4, S. Farrell5, S. Gerland4, D. Perovich6, R. Ricker7, X. Tian-Kunze3, and M. Webster8 1National Snow and Ice Data Center, Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USA 2Earth System Science Interdisciplinary Center, University of Maryland, College
DOI: 10.25923/e8jc-f342 M. -L. Timmermans1 and Z. Labe2 1Yale University, New Haven, CT, USA 2Atmospheric and Oceanic Sciences Program, Princeton University, Princeton, NJ, USA Headlines Arctic Ocean sea surface temperatures (SSTs) in the summer (June-August) are driven by the amount of incoming solar radiation absorbed by the sea surface and by the flow of warm
Sea Surface Temperature Read More »
DOI: 10.25923/nb05-8w13 K. E. Frey1, J. C. Comiso2, L. W. Cooper3, C. Garcia4, J. M. Grebmeier3, and L. V. Stock2 1Graduate School of Geography, Clark University, Worcester, MA, USA 2Cryospheric Sciences Laboratory, Goddard Space Flight Center, NASA, Greenbelt, MD, USA 3Chesapeake Biological Laboratory, University of Maryland Center for Environmental Science, University of Maryland, Solomons, MD,
DOI: 10.25923/s86a-jn24 G. V. Frost1, M. J. Macander1, U. S. Bhatt2, L. T. Berner3, J. W. Bjerke4, H. E. Epstein5, B. C. Forbes6, M. J. Lara7,8, R. Í. Magnússon9, P. M. Montesano10, G. K. Phoenix11, S. P. Serbin12, H. Tømmervik4, C. Waigl13, D. A. Walker14, and D. Yang12,15 1Alaska Biological Research, Inc., Fairbanks, AK, USA
More frequent extreme weather and climate events are transforming the Arctic, yet resiliency and opportunity lie within diverse partnerships The Arctic is increasingly warmer, less frozen, and wetter, with regional extremes in weather, climate patterns, and ecosystem responses. Centering locally and internationally-focused partnerships, long-term observations, and equitable climate solutions provides Arctic communities and nations as
DOI: 10.25923/5vfa-k694 R. L. Thoman1,2, T. A. Moon3, and M. L. Druckenmiller3 1Alaska Center for Climate Assessment and Policy, University of Alaska Fairbanks, Fairbanks, AK, USA 2International Arctic Research Center, University of Alaska Fairbanks, Fairbanks, AK, USA 3National Snow and Ice Data Center, Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder,
2023 Arctic Report Card Arctic Report Card Playlist on YouTube Graphics from Climate.gov Download Arctic Report Card video transcripts and mp4 files from NOAA PMEL’s repository.
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