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  • Articles  (35)
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  • American Association for the Advancement of Science (AAAS)  (35)
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  • 1
    Publication Date: 2014-05-31
    Description: The most prominent pattern in global marine biogeography is the biodiversity peak in the Indo-Australian Archipelago. Yet the processes that underpin this pattern are still actively debated. By reconstructing global marine paleoenvironments over the past 3 million years on the basis of sediment cores, we assessed the extent to which Quaternary climate fluctuations can explain global variation in current reef fish richness. Comparing global historical coral reef habitat availability with the present-day distribution of 6316 reef fish species, we find that distance from stable coral reef habitats during historical periods of habitat loss explains 62% of the variation in fish richness, outweighing present-day environmental factors. Our results highlight the importance of habitat persistence during periods of climate change for preserving marine biodiversity.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Pellissier, Loic -- Leprieur, Fabien -- Parravicini, Valeriano -- Cowman, Peter F -- Kulbicki, Michel -- Litsios, Glenn -- Olsen, Steffen M -- Wisz, Mary S -- Bellwood, David R -- Mouillot, David -- New York, N.Y. -- Science. 2014 May 30;344(6187):1016-9. doi: 10.1126/science.1249853.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉University of Fribourg, Department of Biology, Chemin du Musee 10, CH-1700 Fribourg, Switzerland. Department of Bioscience, Aarhus University, 8000 C Aarhus, Denmark. ; Laboratoire Ecologie des Systemes Marins Cotiers UMR 5119, CNRS, Institut de Recherche pour le Developpement (IRD), Institut Francais de Recherche pour l'Exploitation de la Mer, UM2, UM1, cc 093, Place E. Bataillon, FR-34095 Montpellier Cedex 5, France. ; IRD, UR 227 CoReUs, LABEX (Laboratoire d'Excellence) Corail, Laboratoire Arago, Boite Postale 44, FR-66651 Banyuls/mer, France. CESAB (Centre de Synthese et d'Analyse sur la Biodiversite)-FRB (Fondation pour la Recherche sur la Biodiversite), Immeuble Henri Poincare, Domaine du Petit Arbois, FR-13857 Aix-en-Provence cedex 3, France. ; Centre for Macroevolution and Macroecology, Research School of Biology, Australian National University, Canberra, ACT 0200, Australia. ; IRD, UR 227 CoReUs, LABEX (Laboratoire d'Excellence) Corail, Laboratoire Arago, Boite Postale 44, FR-66651 Banyuls/mer, France. ; Department of Ecology and Evolution, Biophore Building, University of Lausanne, 1015 Lausanne, Switzerland. Swiss Institute of Bioinformatics, Quartier Sorge, 1015 Lausanne, Switzerland. ; Center for Ocean and Ice, Danish Meteorological Institute, Lyngbyvej 100, 2100 Copenhagen, Denmark. ; Department of Bioscience, Aarhus University, 8000 C Aarhus, Denmark. Department of Ecology and Environment, DHI Water and Environment, 2970 Horsholm, Denmark. ; Australian Research Council Centre of Excellence for Coral Reef Studies, and School of Marine and Tropical Biology, James Cook University, Townsville, QLD 4811, Australia. ; Laboratoire Ecologie des Systemes Marins Cotiers UMR 5119, CNRS, Institut de Recherche pour le Developpement (IRD), Institut Francais de Recherche pour l'Exploitation de la Mer, UM2, UM1, cc 093, Place E. Bataillon, FR-34095 Montpellier Cedex 5, France. Australian Research Council Centre of Excellence for Coral Reef Studies, and School of Marine and Tropical Biology, James Cook University, Townsville, QLD 4811, Australia. david.mouillot@univ-montp2.fr.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24876495" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Australia ; *Biodiversity ; *Climate Change ; *Conservation of Natural Resources ; *Coral Reefs ; *Fishes
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 2
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    American Association for the Advancement of Science (AAAS)
    Publication Date: 2014-08-26
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Marshall, Shawn -- New York, N.Y. -- Science. 2014 Aug 22;345(6199):872. doi: 10.1126/science.1258584.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Geography, University of Calgary, Calgary, Alberta, T2N 1N4, Canada. shawn.marshall@ucalgary.ca.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/25146269" target="_blank"〉PubMed〈/a〉
    Keywords: *Climate Change ; *Human Activities ; Humans ; *Ice Cover ; *Oceans and Seas
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 3
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    American Association for the Advancement of Science (AAAS)
    Publication Date: 2014-07-19
    Description: Oceanic transports of heat, salt, fresh water, dissolved CO2, and other tracers regulate global climate change and the distribution of natural marine resources. The time-mean ocean circulation transports fluid as a conveyor belt, but fluid parcels can also be trapped and transported discretely by migrating mesoscale eddies. By combining available satellite altimetry and Argo profiling float data, we showed that the eddy-induced zonal mass transport can reach a total meridionally integrated value of up to 30 to 40 sverdrups (Sv) (1 Sv = 10(6) cubic meters per second), and it occurs mainly in subtropical regions, where the background flows are weak. This transport is comparable in magnitude to that of the large-scale wind- and thermohaline-driven circulation.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Zhang, Zhengguang -- Wang, Wei -- Qiu, Bo -- New York, N.Y. -- Science. 2014 Jul 18;345(6194):322-4. doi: 10.1126/science.1252418. Epub 2014 Jun 26.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Physical Oceanography Lab, Qingdao Collaborative Innovation Center of Marine Science and Technology, Ocean University of China, Qingdao, People's Republic of China. ; Physical Oceanography Lab, Qingdao Collaborative Innovation Center of Marine Science and Technology, Ocean University of China, Qingdao, People's Republic of China. wei@ouc.edu.cn. ; Department of Oceanography, University of Hawaii at Manoa, Honolulu, HI, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/25035491" target="_blank"〉PubMed〈/a〉
    Keywords: *Climate Change ; *Hot Temperature ; Oceans and Seas ; *Water Cycle ; *Water Movements
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 4
    Publication Date: 2014-08-16
    Description: The ongoing global glacier retreat is affecting human societies by causing sea-level rise, changing seasonal water availability, and increasing geohazards. Melting glaciers are an icon of anthropogenic climate change. However, glacier response times are typically decades or longer, which implies that the present-day glacier retreat is a mixed response to past and current natural climate variability and current anthropogenic forcing. Here we show that only 25 +/- 35% of the global glacier mass loss during the period from 1851 to 2010 is attributable to anthropogenic causes. Nevertheless, the anthropogenic signal is detectable with high confidence in glacier mass balance observations during 1991 to 2010, and the anthropogenic fraction of global glacier mass loss during that period has increased to 69 +/- 24%.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Marzeion, Ben -- Cogley, J Graham -- Richter, Kristin -- Parkes, David -- New York, N.Y. -- Science. 2014 Aug 22;345(6199):919-21. doi: 10.1126/science.1254702. Epub 2014 Aug 14.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Institute of Meteorology and Geophysics, University of Innsbruck, Austria. ben.marzeion@uibk.ac.at. ; Department of Geography, Trent University, Peterborough, Canada. ; Institute of Meteorology and Geophysics, University of Innsbruck, Austria.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/25123485" target="_blank"〉PubMed〈/a〉
    Keywords: Climate ; *Climate Change ; Freezing ; *Human Activities ; Humans ; *Ice Cover ; *Oceans and Seas
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 5
    Publication Date: 2014-02-08
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Kerr, Richard A -- New York, N.Y. -- Science. 2014 Feb 7;343(6171):588. doi: 10.1126/science.343.6171.588.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24503825" target="_blank"〉PubMed〈/a〉
    Keywords: *Air Movements ; *Climate Change
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 6
    Publication Date: 2014-07-06
    Description: In 1990, Andrew Bakun proposed that increasing greenhouse gas concentrations would force intensification of upwelling-favorable winds in eastern boundary current systems that contribute substantial services to society. Because there is considerable disagreement about whether contemporary wind trends support Bakun's hypothesis, we performed a meta-analysis of the literature on upwelling-favorable wind intensification. The preponderance of published analyses suggests that winds have intensified in the California, Benguela, and Humboldt upwelling systems and weakened in the Iberian system over time scales ranging up to 60 years; wind change is equivocal in the Canary system. Stronger intensification signals are observed at higher latitudes, consistent with the warming pattern associated with climate change. Overall, reported changes in coastal winds, although subtle and spatially variable, support Bakun's hypothesis of upwelling intensification in eastern boundary current systems.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Sydeman, W J -- Garcia-Reyes, M -- Schoeman, D S -- Rykaczewski, R R -- Thompson, S A -- Black, B A -- Bograd, S J -- New York, N.Y. -- Science. 2014 Jul 4;345(6192):77-80. doi: 10.1126/science.1251635.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Farallon Institute for Advanced Ecosystem Research, Suite Q, 101 H Street, Petaluma, CA 94952, USA. wsydeman@comcast.net. ; Farallon Institute for Advanced Ecosystem Research, Suite Q, 101 H Street, Petaluma, CA 94952, USA. ; Faculty of Science, Health, Education and Engineering, University of the Sunshine Coast, Locked Bag 4, Maroochydore DC, Queensland 4558, Australia. ; Department of Biological Sciences and Marine Science Program, University of South Carolina, 701 Sumter Street, Columbia, SC 29208, USA. ; Farallon Institute for Advanced Ecosystem Research, Suite Q, 101 H Street, Petaluma, CA 94952, USA. Climate Impacts Group, University of Washington, Box 355674, Seattle, WA 98195, USA. ; Marine Science Institute, University of Texas, 750 Channel View Drive, Port Aransas, TX 78373, USA. ; Environmental Research Division, National Oceanic and Atmospheric Administration (NOAA) Southwest Fisheries Science Center, 1352 Lighthouse Avenue, Pacific Grove, CA 93950-2097, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24994651" target="_blank"〉PubMed〈/a〉
    Keywords: California ; *Climate Change ; *Ecosystem ; Greenhouse Effect ; *Wind
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    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 7
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    American Association for the Advancement of Science (AAAS)
    Publication Date: 2014-08-16
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Rau, Greg H -- New York, N.Y. -- Science. 2014 Aug 15;345(6198):739. doi: 10.1126/science.345.6198.739-c. Epub 2014 Aug 14.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Institute of Marine Sciences, University of California, Santa Cruz, CA 95064, USA. ghrau@sbcglobal.net.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/25124418" target="_blank"〉PubMed〈/a〉
    Keywords: *Administrative Personnel ; *Climate Change ; Humans
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    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 8
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    American Association for the Advancement of Science (AAAS)
    Publication Date: 2014-02-01
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Nisbet, Euan G -- Dlugokencky, Edward J -- Bousquet, Philippe -- New York, N.Y. -- Science. 2014 Jan 31;343(6170):493-5. doi: 10.1126/science.1247828.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Earth Sciences, Royal Holloway, University of London, Egham TW20 0EX, UK.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24482471" target="_blank"〉PubMed〈/a〉
    Keywords: Air ; Atmosphere/*chemistry ; *Climate Change ; Coal ; Geography ; Greenhouse Effect/prevention & control ; Humans ; Industry ; Methane/*analysis ; Seasons ; Wetlands
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    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 9
    Publication Date: 2014-01-05
    Description: Pine Island Glacier has thinned and accelerated over recent decades, significantly contributing to global sea-level rise. Increased oceanic melting of its ice shelf is thought to have triggered those changes. Observations and numerical modeling reveal large fluctuations in the ocean heat available in the adjacent bay and enhanced sensitivity of ice-shelf melting to water temperatures at intermediate depth, as a seabed ridge blocks the deepest and warmest waters from reaching the thickest ice. Oceanic melting decreased by 50% between January 2010 and 2012, with ocean conditions in 2012 partly attributable to atmospheric forcing associated with a strong La Nina event. Both atmospheric variability and local ice shelf and seabed geometry play fundamental roles in determining the response of the Antarctic Ice Sheet to climate.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Dutrieux, Pierre -- De Rydt, Jan -- Jenkins, Adrian -- Holland, Paul R -- Ha, Ho Kyung -- Lee, Sang Hoon -- Steig, Eric J -- Ding, Qinghua -- Abrahamsen, E Povl -- Schroder, Michael -- New York, N.Y. -- Science. 2014 Jan 10;343(6167):174-8. doi: 10.1126/science.1244341. Epub 2014 Jan 2.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉British Antarctic Survey, Natural Environment Research Council (NERC), Cambridge, UK.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24385606" target="_blank"〉PubMed〈/a〉
    Keywords: *Climate Change ; Freezing ; *Ice Cover ; *Islands
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    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 10
    Publication Date: 2014-09-06
    Description: Greenland ice core water isotopic composition (delta(18)O) provides detailed evidence for abrupt climate changes but is by itself insufficient for quantitative reconstruction of past temperatures and their spatial patterns. We investigate Greenland temperature evolution during the last deglaciation using independent reconstructions from three ice cores and simulations with a coupled ocean-atmosphere climate model. Contrary to the traditional delta(18)O interpretation, the Younger Dryas period was 4.5 degrees +/- 2 degrees C warmer than the Oldest Dryas, due to increased carbon dioxide forcing and summer insolation. The magnitude of abrupt temperature changes is larger in central Greenland (9 degrees to 14 degrees C) than in the northwest (5 degrees to 9 degrees C), fingerprinting a North Atlantic origin. Simulated changes in temperature seasonality closely track changes in the Atlantic overturning strength and support the hypothesis that abrupt climate change is mostly a winter phenomenon.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Buizert, Christo -- Gkinis, Vasileios -- Severinghaus, Jeffrey P -- He, Feng -- Lecavalier, Benoit S -- Kindler, Philippe -- Leuenberger, Markus -- Carlson, Anders E -- Vinther, Bo -- Masson-Delmotte, Valerie -- White, James W C -- Liu, Zhengyu -- Otto-Bliesner, Bette -- Brook, Edward J -- New York, N.Y. -- Science. 2014 Sep 5;345(6201):1177-80. doi: 10.1126/science.1254961.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA. buizertc@science.oregonstate.edu. ; Centre for Ice and Climate, Niels Bohr Institute, University of Copenhagen, Denmark. Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO 80309, USA. ; Scripps Institution of Oceanography, University of California-San Diego, La Jolla, CA 92093, USA. ; Center for Climatic Research, Nelson Institute for Environmental Studies, University of Wisconsin, Madison, WI 53706, USA. ; Department of Physics and Physical Oceanography, Memorial University, St. John's, Canada. ; Division of Climate and Environmental Physics, Physics Institute and Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland. ; College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA. ; Centre for Ice and Climate, Niels Bohr Institute, University of Copenhagen, Denmark. ; Laboratoire des Sciences du Climat et de l'Environnement, Institut Pierre Simon Laplace (UMR CEA-CNRS-UVSQ 8212), Gif-sur-Yvette, France. ; Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO 80309, USA. ; Center for Climatic Research, Nelson Institute for Environmental Studies, University of Wisconsin, Madison, WI 53706, USA. Laboratory for Climate and Ocean-Atmosphere Studies, Peking University, Beijing 100871, China. ; Climate and Global Dynamics Division, National Center for Atmospheric Research, Boulder, CO 80307, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/25190795" target="_blank"〉PubMed〈/a〉
    Keywords: *Climate Change ; Computer Simulation ; Freezing ; Greenland ; *Ice Cover ; Models, Theoretical ; Oxygen Isotopes/analysis ; *Temperature
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    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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