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机译:全球海洋表层海洋pCO_2的气候平均值和年代际变化以及海洋净空气CO_2通量
Lamont-Doherty Earth Observatory, Columbia University, 61 Route 9W, PO Box 1000, Palisades, NY 10964-8000, USA;
Lamont-Doherty Earth Observatory, Columbia University, 61 Route 9W, PO Box 1000, Palisades, NY 10964-8000, USA;
Atlantic Oceanographic and Meteorological Laboratory, National Oceanographic and Atmospheric Administration, Miami, FL, USA;
Earth System Research Laboratory, National Oceanographic and Atmospheric Administration, Boulder, CO, USA;
Pacific Marine Environmental Laboratory, National Oceanographic and Atmospheric Administration, Seattle, WA, USA;
103 Reach Road, Harpswell, ME, USA;
College of Oceanic and Atmospheric Sciences, Oregon State University, Corvallis, OR, USA;
Monterey Bay Aquarium Research Institute, Moss Landing, CA, USA;
Monterey Bay Aquarium Research Institute, Moss Landing, CA, USA;
Pacific Marine Environmental Laboratory, National Oceanographic and Atmospheric Administration, Seattle, WA, USA;
School of Environmental Sciences, University of East Anglia, Norwich, UK;
School of Environmental Sciences, University of East Anglia, Norwich, UK;
School of Environmental Sciences, University of East Anglia, Norwich, UK;
Laboratoire d'Oceanographie et du Climat, LOCEAN/IPSL, CNRS. Universite Pierre et Marie Curie, Paris, France;
Graduate School of Environmental Earth Science, Hokkaido University, Sapporo, Japan;
Meteorological Research Institute, Tsukuba, Japan;
Meteorological Research Institute, Tsukuba, Japan;
National Institute for Environmental Studies, Tsukuba, Japan;
Leibniz Institute of Marine Sciences, Kiel, Germany;
Leibniz Institute of Marine Sciences, Kiel, Germany;
Alfred Wegener Institute, Bremerhaven, Germany;
Marine Research Institute and University of Iceland, Reykjavik, Iceland;
Marine Research Institute and University of Iceland, Reykjavik, Iceland;
Wealth from Oceans, CSIRO National Research Flagship, and the Antarctic Climate and Ecosystem Cooperative Research Center, Hobart, Australia;
Bjerknes Centre for Climate Research, University of Bergen, Norway;
Bjerknes Centre for Climate Research, University of Bergen, Norway;
Bjerknes Centre for Climate Research, University of Bergen, Norway;
Institute of Ocean Sciences, Fisheries and Oceans Canada, Sidney, B.C., Canada;
Universite de Liege, Liege, Belgium;
Bermuda Institute of Ocean Studies, Bermuda;
Royal Netherlands Institute of Sea Research, Den Burg, The Netherlands;
carbon dioxide; partial pressure; surface ocean; global ocean; sea-air flux;
机译:气候风,海洋pCO_2和气体传输算法中的不确定性对全球海洋空气CO_2通量估算的影响
机译:在简化的生物地球化学离线模型中,利用船舶对海洋表层pCO_2的观测,对全球海洋pCO_2和海气CO_2通量进行模拟和同化
机译:观测驱动海洋混合层方案的全球表面海洋p〜(CO_2)和海洋CO_2通量变化
机译:热带太平洋海洋pCO_2和海气CO_2通量的变化
机译:来自遥感的全球海洋潜热通量的最新变化。
机译:城市二氧化碳排放对近岸海域空气通量和海洋酸化的影响
机译:海洋调节了全球气候对自然和人为强迫的响应。然而,在过去的2,000年中(这是了解当前和未来气候对这些强迫的响应的关键间隔),全球海表温度变化及其潜在的驱动机制受到的约束很有限。在这里,我们提出了一个共同的时期(ce)的全球海面温度的全球综合,该综合来自57个符合严格质量控制标准的海洋重建项目。我们观察到从1到1800 ce的冷却趋势,对于显式测试重建中潜在的偏倚而言,该趋势很稳健。在801至1800 ce之间,表面降温趋势在质量上与地面温度重建的独立合成以及从使用过去外部辐射强迫的最佳估计的气候模型模拟集合推导出的海面温度合成在质量上是一致的。使用单一和累积强迫的气候模拟表明,从801到1800 ce的海洋表面冷却趋势主要不是对轨道强迫的反应,而是爆炸性火山爆发的频繁发生。我们的结果表明,火山喷发的反复簇可引起净的负辐射强迫,这会导致混合层海洋热量降低而导致百年和全球规模的降温趋势。
机译:全球海洋表面热通量气候学的不确定性来自船舶观测