Arctic Report Card 2020 the Sustained Transformation to a Warmer, Less Frozen and Biologically Changed Arctic Remains Clear
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Meltwater Routing and the Younger Dryas
Meltwater routing and the Younger Dryas Alan Condrona,1 and Peter Winsorb aClimate System Research Center, Department of Geosciences, University of Massachusetts, Amherst, MA 01003; and bInstitute of Marine Science, School of Fisheries and Ocean Sciences, University of Alaska Fairbanks, Fairbanks, AK 99775 Edited by James P. Kennett, University of California, Santa Barbara, CA, and approved September 27, 2012 (received for review May 2, 2012) The Younger Dryas—the last major cold episode on Earth—is gen- to correct another. A separate reconstruction of the drainage erally considered to have been triggered by a meltwater flood into chronology of North America by Tarasov and Peltier (8) found the North Atlantic. The prevailing hypothesis, proposed by Broecker that rather than being to the east, the geographical release point of et al. [1989 Nature 341:318–321] more than two decades ago, sug- meltwater to the ocean at this time might have been toward the gests that an abrupt rerouting of Lake Agassiz overflow through Arctic. Further support for a northward drainage route has since the Great Lakes and St. Lawrence Valley inhibited deep water for- been provided by Peltier et al. (9). Using a numerical model, the mation in the subpolar North Atlantic and weakened the strength authors showed that the response of the AMOC to meltwater of the Atlantic Meridional Overturning Circulation (AMOC). More re- placed directly over the North Atlantic (50° N to 70° N) and the cently, Tarasov and Peltier [2005 Nature 435:662–665] showed that entire Arctic Ocean were almost identical. This result implies that meltwater could have discharged into the Arctic Ocean via the meltwater released into the Arctic might be capable of cooling the Mackenzie Valley ∼4,000 km northwest of the St. -
Baffin Bay Sea Ice Extent and Synoptic Moisture Transport Drive Water Vapor
Atmos. Chem. Phys., 20, 13929–13955, 2020 https://doi.org/10.5194/acp-20-13929-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Baffin Bay sea ice extent and synoptic moisture transport drive water vapor isotope (δ18O, δ2H, and deuterium excess) variability in coastal northwest Greenland Pete D. Akers1, Ben G. Kopec2, Kyle S. Mattingly3, Eric S. Klein4, Douglas Causey2, and Jeffrey M. Welker2,5,6 1Institut des Géosciences et l’Environnement, CNRS, 38400 Saint Martin d’Hères, France 2Department of Biological Sciences, University of Alaska Anchorage, 99508 Anchorage, AK, USA 3Institute of Earth, Ocean, and Atmospheric Sciences, Rutgers University, 08854 Piscataway, NJ, USA 4Department of Geological Sciences, University of Alaska Anchorage, 99508 Anchorage, AK, USA 5Ecology and Genetics Research Unit, University of Oulu, 90014 Oulu, Finland 6University of the Arctic (UArctic), c/o University of Lapland, 96101 Rovaniemi, Finland Correspondence: Pete D. Akers ([email protected]) Received: 9 April 2020 – Discussion started: 18 May 2020 Revised: 23 August 2020 – Accepted: 11 September 2020 – Published: 19 November 2020 Abstract. At Thule Air Base on the coast of Baffin Bay breeze development, that radically alter the nature of rela- (76.51◦ N, 68.74◦ W), we continuously measured water va- tionships between isotopes and many meteorological vari- por isotopes (δ18O, δ2H) at a high frequency (1 s−1) from ables in summer. On synoptic timescales, enhanced southerly August 2017 through August 2019. Our resulting record, flow promoted by negative NAO conditions produces higher including derived deuterium excess (dxs) values, allows an δ18O and δ2H values and lower dxs values. -
Ecological Consequences of Sea-Ice Decline Eric Post Et Al
SPECIALSECTION 31. K. B. Ritchie, Mar. Ecol. Prog. Ser. 322,1–14 (2006). 52. C. Moritz, R. Agudo, Science 341, 504–508 (2013). 71. A. J. McMichael, Proc. Natl. Acad. Sci. U.S.A. 109, 32. B. Humair et al., ISME J. 3, 955–965 (2009). 53. C. D. Thomas et al., Nature 427, 145–148 4730–4737 (2012). 33. D. Corsaro, G. Greub, Clin. Microbiol. Rev. 19,283–297 (2006). (2004). 72. T. Wheeler, J. von Braun, Science 341, 508–513 34. W. Jetz et al., PLoS Biol. 5, e157 (2007). 54. Intergovernmental Panel on Climate Change, Summary (2013). 35. B. J. Cardinale et al., Nature 486,59–67 (2012). for Policymakers. Climate Change 2007: The Physical 73. S. S. Myers, J. A. Patz, Annu. Rev. Environ. Resour. 34, 36. P. T. J. Johnson, J. T. Hoverman, Proc. Natl. Acad. Sci. U.S.A. Science Basis. Contribution of Working Group I to the Fourth 223–252 (2009). 109,9006–9011 (2012). Assessment Report of the Intergovernmental Panel on 74. C. A. Deutsch et al., Proc. Natl. Acad. Sci. U.S.A. 105, 37. F. Keesing et al., Nature 468, 647–652 (2010). Climate Change (Cambridge Univ. Press, New York, 2007). 6668–6672 (2008). 38. P. H. Hobbelen, M. D. Samuel, D. Foote, L. Tango, 55. S. Laaksonen et al., EcoHealth 7,7–13 (2010). D. A. LaPointe, Theor. Ecol. 6,31–44 (2013). 56. O. Gilg et al., Ann. N. Y. Acad. Sci. 1249, 166–190 (2012). Acknowledgments: This work was supported in part by an NSF 39. T. -
Oregon State University Insert PDF 480 K
ARCTIC Arctic Research Consortium of the United States Member Institution Winter 2004/2005, Volume 11 Number 2 Arctic Research at Oregon State University land grant university, Oregon State Geosciences A University was designated as Oregon’s state-assisted agricultural college in 1868. Polar Ice Cores Sea grant and space grant designation came Ed Brook (Geosciences) applies geochemical techniques to diverse problems in late Quater- later, making OSU one of only six universi- nary paleoclimatology; several of his projects have arctic components. NSF-supported work ties to have all three titles. OSU currently focused on the relative timing of millennial-scale abrupt climate change in Greenland and enrolls 15,599 undergraduate and 3,380 Antarctica uses atmospheric methane and the isotopic composition of oxygen as correlation graduate students in more than 200 under- tools to place climate records from the Siple Dome (west Antarctica) and GISP2 (Green- graduate and 80 graduate degree programs. land) ice cores on a precise common chronology for the period from 9–57 ka. The onset With collaborative connections across of major millennial warming events in Siple Dome precedes major abrupt warmings in the globe, OSU researchers contribute to Greenland, and the pattern of millennial change at Siple Dome is broadly similar, though arctic research from disciplines housed in not identical, to that previously observed for the Byrd ice core (also in west Antarctica). a variety of colleges. The College of Oce- The addition of Siple Dome to the database of well-dated Antarctic paleoclimate records anic and Atmospheric Sciences (COAS) supports the case for a regionally consistent pattern of millennial-scale climate change in has several researchers working on arctic Antarctica during the last ice age and glacial-interglacial transition. -
New Facts and Additional Information Supporting the Cop16
NOVEMBER 2012 NRDC ISSUE PAPER IP:12-11-A New Facts and Additional Information Supporting the CoP16 Polar Bear Proposal Submitted by the United States of America About NRDC NRDC (Natural Resources Defense Council) is a national nonprofit environmental organization with more than 1.3 million members and online activists. Since 1970, our lawyers, scientists, and other environmental specialists have worked to protect the world’s natural resources, public health, and the environment. NRDC has offices in New York City, Washington, D.C., Los Angeles, San Francisco, Chicago, Montana, and Beijing. Visit us at www.nrdc.org. NRDC’s policy publications aim to inform and influence solutions to the world’s most pressing environmental and public health issues. For additional policy content, visit our online policy portal at www.nrdc.org/policy. NRDC Director of Communications: Phil Gutis NRDC Deputy Director of Communications: Lisa Goffredi NRDC Policy Publications Director: Alex Kennaugh Lead Editor: Design and Production: www.suerossi.com Cover photo © Paul Shoul: paulshoulphotography.com © Natural Resources Defense Council 2012 n October 4, 2012, the United States, supported by the Russian Federation, submitted a proposal to transfer the polar bear, Ursus maritimus, from OAppendix II to Appendix I of the Convention in accordance with Article II and Resolution Conf. 9.24 (Rev. CoP15) on the basis that the polar bear is affected by trade and shows a marked decline in the population size in the wild, which has been inferred or projected on the basis of a decrease in area of habitat and a decrease in quality of habitat. Pursuant to the Convention, “Appendix I shall include all species threatened with extinction which are or may be affected by trade.” CITES Article II, paragraph 1. -
Modelling the Transfer of Supraglacial Meltwater to the Bed of Leverett Glacier, Southwest Greenland
The Cryosphere, 9, 123–138, 2015 www.the-cryosphere.net/9/123/2015/ doi:10.5194/tc-9-123-2015 © Author(s) 2015. CC Attribution 3.0 License. Modelling the transfer of supraglacial meltwater to the bed of Leverett Glacier, Southwest Greenland C. C. Clason1, D. W. F. Mair2, P. W. Nienow3, I. D. Bartholomew3, A. Sole4, S. Palmer5, and W. Schwanghart6 1Department of Physical Geography and Quaternary Geology, Stockholm University, 106 91 Stockholm, Sweden 2Geography and Environment, University of Aberdeen, Aberdeen, AB24 3UF, UK 3School of Geosciences, University of Edinburgh, Edinburgh, EH8 9XP, UK 4Department of Geography, University of Sheffield, Sheffield, S10 2TN, UK 5Geography, College of Life and Environmental Sciences, University of Exeter, Exeter, EX4 4RJ, UK 6Institute of Earth and Environmental Science, University of Potsdam, 14476 Potsdam-Golm, Germany Correspondence to: C. C. Clason ([email protected]) Received: 23 June 2014 – Published in The Cryosphere Discuss.: 29 July 2014 Revised: 12 December 2014 – Accepted: 24 December 2014 – Published: 22 January 2015 Abstract. Meltwater delivered to the bed of the Greenland melt to the bed matches the observed delay between the peak Ice Sheet is a driver of variable ice-motion through changes air temperatures and subsequent velocity speed-ups, while in effective pressure and enhanced basal lubrication. Ice sur- the instantaneous transfer of melt to the bed in a control sim- face velocities have been shown to respond rapidly both ulation does not. Although both moulins and lake drainages to meltwater production at the surface and to drainage of are predicted to increase in number for future warmer climate supraglacial lakes, suggesting efficient transfer of meltwa- scenarios, the lake drainages play an increasingly important ter from the supraglacial to subglacial hydrological systems. -
Recent Declines in Warming and Vegetation Greening Trends Over Pan-Arctic Tundra
Remote Sens. 2013, 5, 4229-4254; doi:10.3390/rs5094229 OPEN ACCESS Remote Sensing ISSN 2072-4292 www.mdpi.com/journal/remotesensing Article Recent Declines in Warming and Vegetation Greening Trends over Pan-Arctic Tundra Uma S. Bhatt 1,*, Donald A. Walker 2, Martha K. Raynolds 2, Peter A. Bieniek 1,3, Howard E. Epstein 4, Josefino C. Comiso 5, Jorge E. Pinzon 6, Compton J. Tucker 6 and Igor V. Polyakov 3 1 Geophysical Institute, Department of Atmospheric Sciences, College of Natural Science and Mathematics, University of Alaska Fairbanks, 903 Koyukuk Dr., Fairbanks, AK 99775, USA; E-Mail: [email protected] 2 Institute of Arctic Biology, Department of Biology and Wildlife, College of Natural Science and Mathematics, University of Alaska, Fairbanks, P.O. Box 757000, Fairbanks, AK 99775, USA; E-Mails: [email protected] (D.A.W.); [email protected] (M.K.R.) 3 International Arctic Research Center, Department of Atmospheric Sciences, College of Natural Science and Mathematics, 930 Koyukuk Dr., Fairbanks, AK 99775, USA; E-Mail: [email protected] 4 Department of Environmental Sciences, University of Virginia, 291 McCormick Rd., Charlottesville, VA 22904, USA; E-Mail: [email protected] 5 Cryospheric Sciences Branch, NASA Goddard Space Flight Center, Code 614.1, Greenbelt, MD 20771, USA; E-Mail: [email protected] 6 Biospheric Science Branch, NASA Goddard Space Flight Center, Code 614.1, Greenbelt, MD 20771, USA; E-Mails: [email protected] (J.E.P.); [email protected] (C.J.T.) * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +1-907-474-2662; Fax: +1-907-474-2473. -
AMAP Update on Selected Climate Issues of Concern: Observations, Short-Lived Climate Forcers, Arctic Carbon Cycle, and Predictive Capability
DRAFT: FOR RESTRICTED CIRCULATION FOR REVIEW PURPOSES ONLY. DO NO CITE, COPY OR DISTRIBUTE Version approved by AMAP WG, 14 January 2009 AMAP Update on Selected Climate Issues of Concern: Observations, Short-lived Climate Forcers, Arctic Carbon Cycle, and Predictive Capability EXECUTIVE SUMMARY C1. The Arctic Climate Impact Assessment and the Intergovernmental Panel on Climate Change have established the importance of climate change in the Arctic both regionally and globally. Following those reports, emphasis has been placed on continued observations, a new assessment of the Arctic carbon cycle, the role of short lived climate forcers in the Arctic, and the need for improved predictive capacity at the regional level in the Arctic. C2. The Arctic continues to warm. Since publication of the Arctic Climate Impact Assessment in 2005, several indicators show further and extensive climate change at rates faster than previously anticipated. Air temperatures are increasing in the Arctic. Sea ice extent has decreased sharply, with a record low in 2007 and ice-free conditions in both the Northeast and Northwest sea passages for first time in recorded history in 2008. As ice that persists for several years (multi- year ice) is replaced by newly formed (first-year) ice, the Arctic sea-ice is becoming increasingly vulnerable to melting. Surface waters in the Arctic Ocean are warming. Permafrost is warming and, at its margins, thawing. Snow cover in the Northern Hemisphere is decreasing by 1-2% per year. Glaciers are shrinking and the melt area of the Greenland Ice Cap is increasing. The treeline is moving northwards in some areas up to 3-10 meters per year, and there is increased shrub growth north of the treeline. -
Safeguarding the Arctic Why the U.S
Safeguarding the Arctic Why the U.S. Must Lead in the High North By Cathleen Kelly and Miranda Peterson January 22, 2015 “As the United States assumes the Chairmanship of the Arctic Council, it is more important than ever that we have a coordinated national effort that takes advantage of our combined expertise and efforts in the Arctic region to promote our shared values and priorities.” — President Obama, Executive Order on Enhancing Coordination of National Efforts in the Arctic, January 21, 20151 While many Americans do not consider the United States to be an Arctic nation, Alaska—which constitutes 16 percent of the country’s landmass and sits on the Arctic Circle—puts the country solidly in that category.2 Consequently, it is with good reason that the United States has a seat on the Arctic Council. As Arctic warming accelerates, U.S. leadership in the High North is key not only to the public health and safety of Americans and other people in the region, but also to U.S. national security and the fate of the planet. In just three months, U.S. Secretary of State John Kerry will become chairman of the Arctic Council. The two-year position rotates among the eight Arctic nations3—Canada, Finland, Iceland, Norway, Russia, Sweden, the United States, and Denmark, including Greenland and the Faroe Islands—and is a powerful platform for shaping how the risks and opportunities of increasing commercial activity at the top of the world are managed. To ready the administration for Secretary Kerry’s turn to hold the Arctic Council gavel from 2015 to 2017, President Barack Obama recently issued an executive order to better coordinate national efforts in the Arctic.4 The executive order is the latest signal from the White House that President Obama and Secretary Kerry are focused on preparing the nation for dramatic changes in the Arctic and protecting U.S. -
Arctic Climate Change Implications for U.S
Arctic Climate Change Implications for U.S. National Security Perspective - Laura Leddy September 2020 i BOARD OF DIRECTORS The Honorable Gary Hart, Chairman Emeritus Scott Gilbert Senator Hart served the State of Colorado in the U.S. Senate Scott Gilbert is a Partner of Gilbert LLP and Managing and was a member of the Committee on Armed Services Director of Reneo LLC. during his tenure. Vice Admiral Lee Gunn, USN (Ret.) Governor Christine Todd Whitman, Chairperson Vice Admiral Gunn is Vice Chairman of the CNA Military Christine Todd Whitman is the President of the Whitman Advisory Board, Former Inspector General of the Department Strategy Group, a consulting firm that specializes in energy of the Navy, and Former President of the Institute of Public and environmental issues. Research at the CNA Corporation. The Honorable Chuck Hagel Brigadier General Stephen A. Cheney, USMC (Ret.), Chuck Hagel served as the 24th U.S. Secretary of Defense and President of ASP served two terms in the United States Senate (1997-2009). Hagel Brigadier General Cheney is the President of ASP. was a senior member of the Senate Foreign Relations; Banking, Housing and Urban Affairs; and Intelligence Committees. Matthew Bergman Lieutenant General Claudia Kennedy, USA (Ret.) Matthew Bergman is an attorney, philanthropist and Lieutenant General Kennedy was the first woman entrepreneur based in Seattle. He serves as a Trustee of Reed to achieve the rank of three-star general in the United States College on the Board of Visitors of Lewis & Clark Law Army. School. Ambassador Jeffrey Bleich The Honorable John F. Kerry The Hon. -
A Spatial Evaluation of Arctic Sea Ice and Regional Limitations in CMIP6 Historical Simulations
1AUGUST 2021 W A T T S E T A L . 6399 A Spatial Evaluation of Arctic Sea Ice and Regional Limitations in CMIP6 Historical Simulations a a a a MATTHEW WATTS, WIESLAW MASLOWSKI, YOUNJOO J. LEE, JACLYN CLEMENT KINNEY, AND b ROBERT OSINSKI a Department of Oceanography, Naval Postgraduate School, Monterey, California b Institute of Oceanology of Polish Academy of Sciences, Sopot, Poland (Manuscript received 29 June 2020, in final form 28 April 2021) ABSTRACT: The Arctic sea ice response to a warming climate is assessed in a subset of models participating in phase 6 of the Coupled Model Intercomparison Project (CMIP6), using several metrics in comparison with satellite observations and results from the Pan-Arctic Ice Ocean Modeling and Assimilation System and the Regional Arctic System Model. Our study examines the historical representation of sea ice extent, volume, and thickness using spatial analysis metrics, such as the integrated ice edge error, Brier score, and spatial probability score. We find that the CMIP6 multimodel mean captures the mean annual cycle and 1979–2014 sea ice trends remarkably well. However, individual models experience a wide range of uncertainty in the spatial distribution of sea ice when compared against satellite measurements and reanalysis data. Our metrics expose common and individual regional model biases, which sea ice temporal analyses alone do not capture. We identify large ice edge and ice thickness errors in Arctic subregions, implying possible model specific limitations in or lack of representation of some key physical processes. We postulate that many of them could be related to the oceanic forcing, especially in the marginal and shelf seas, where seasonal sea ice changes are not adequately simulated. -
Thinking About the Arctic's Future
By Lawson W. Brigham ThinkingThinking aboutabout thethe Arctic’sArctic’s Future:Future: ScenariosScenarios forfor 20402040 MIKE DUNN / NOAA CLIMATE PROGRAM OFFICE, NABOS 2006 EXPEDITION The warming of the Arctic could These changes have profound con- ing in each of the four scenarios. mean more circumpolar sequences for the indigenous people, • Transportation systems, espe- for all Arctic species and ecosystems, cially increases in marine and air transportation and access for and for any anticipated economic access. the rest of the world—but also development. The Arctic is also un- • Resource development—for ex- an increased likelihood of derstood to be a large storehouse of ample, oil and gas, minerals, fish- yet-untapped natural resources, a eries, freshwater, and forestry. overexploited natural situation that is changing rapidly as • Indigenous Arctic peoples— resources and surges of exploration and development accel- their economic status and the im- environmental refugees. erate in places like the Russian pacts of change on their well-being. Arctic. • Regional environmental degra- The combination of these two ma- dation and environmental protection The Arctic is undergoing an jor forces—intense climate change schemes. extraordinary transformation early and increasing natural-resource de- • The Arctic Council and other co- in the twenty-first century—a trans- velopment—can transform this once- operative arrangements of the Arctic formation that will have global im- remote area into a new region of im- states and those of the regional and pacts. Temperatures in the Arctic are portance to the global economy. To local governments. rising at unprecedented rates and evaluate the potential impacts of • Overall geopolitical issues fac- are likely to continue increasing such rapid changes, we turn to the ing the region, such as the Law of throughout the century.