Zobrazeno 1 - 10 of 1 036 pro vyhledávání: '"Haywood AM"'
1
Akademický článek
Highly restricted near-surface permafrost extent during the mid-Pliocene warm period.
Autor: Guo D; Nansen-Zhu International Research Centre, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China.; Key Laboratory of Meteorological Disaster, Ministry of Education/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science and Technology, Nanjing 210044, China., Wang H; Key Laboratory of Meteorological Disaster, Ministry of Education/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science and Technology, Nanjing 210044, China., Romanovsky VE; Geophysical Institute, University of Alaska Fairbanks, Fairbanks, AK 99775.; Earth Cryosphere Institute, Tyumen Scientific Centre, Siberian Branch of the Russian Academy of Science, Tyumen 625026, Russia., Haywood AM; School of Earth and Environment, University of Leeds, Leeds LS2 9JT, United Kingdom., Pepin N; School of Environment, Geography and Geosciences, University of Portsmouth, Portsmouth PO1 3HE, United Kingdom., Salzmann U; Department of Geography and Environmental Sciences, Northumbria University, Newcastle upon Tyne NE1 8ST, United Kingdom., Sun J; Nansen-Zhu International Research Centre, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China., Yan Q; Nansen-Zhu International Research Centre, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China., Zhang Z; Department of Atmospheric Science, School of Environmental Studies, China University of Geoscience, Wuhan 430074, China., Li X; Department of Atmospheric Science, School of Environmental Studies, China University of Geoscience, Wuhan 430074, China., Otto-Bliesner BL; Climate and Global Dynamics Laboratory, National Center for Atmospheric Research, Boulder, CO 80307., Feng R; Department of Earth Sciences, University of Connecticut, Storrs, CT 06269., Lohmann G; Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven 27570, Germany., Stepanek C; Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven 27570, Germany., Abe-Ouchi A; Atmosphere and Ocean Research Institute, University of Tokyo, Kashiwa 277-8568, Japan., Chan WL; Atmosphere and Ocean Research Institute, University of Tokyo, Kashiwa 277-8568, Japan., Peltier WR; Department of Physics, University of Toronto, Toronto M5S 1A7, Canada., Chandan D; Department of Physics, University of Toronto, Toronto M5S 1A7, Canada., von der Heydt AS; Institute for Marine and Atmospheric Research Utrecht, Department of Physics, Utrecht University, Utrecht 3584 CC, The Netherlands., Contoux C; Laboratoire des Sciences du Climat et de l'Environnement/Institut Pierre Simon Laplace, Commissariat à l'Energie Atomique-Centre National de la Recherche Scientifique-Université de Versailles Saint Quentin, Université Paris-Saclay, Gif-sur-Yvette 91191, France., Chandler MA; Center for Climate Systems Research, Columbia University, New York, NY 10025.; Goddard Institute for Space Studies, National Aeronautics and Space Administration, New York, NY 10025., Tan N; Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China., Zhang Q; Department of Physical Geography and Bolin Centre for Climate Research, Stockholm University, Stockholm 10691, Sweden., Hunter SJ; School of Earth and Environment, University of Leeds, Leeds LS2 9JT, United Kingdom., Kamae Y; Faculty of Life and Environmental Sciences, University of Tsukuba, Tsukuba 305-8572, Japan.
Publikováno v: Proceedings of the National Academy of Sciences of the United States of America [Proc Natl Acad Sci U S A] 2023 Sep 05; Vol. 120 (36), pp. e2301954120. Date of Electronic Publication: 2023 Aug 28.
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2
Mid-Pliocene West African Monsoon rainfall as simulated in the PlioMIP2 ensemble
Autor: Berntell, E, Zhang, Q, Li, Q, Haywood, AM, Tindall, JC, Hunter, SJ, Zhang, Z, Li, X, Guo, C, Nisancioglu, KH, Stepanek, C, Lohmann, G, Sohl, LE, Chandler, MA, Tan, N, Contoux, C, Ramstein, G, Baatsen, MLJ, von der Heydt, AS, Chandan, D, Peltier, WR, Abe-Ouchi, A, Chan, W-L, Kamae, Y, Williams, CJR, Lunt, DJ, Feng, R, Otto-Bliesner, BL, Brady, EC
Publikováno v: Climate of the Past
Climate of the Past, European Geosciences Union (EGU), 2021, 17 (4), pp.1777-1794. ⟨10.5194/cp-17-1777-2021⟩
Berntell, E, Zhang, Q, Li, Q, Haywood, A M, Tindall, J C, Hunter, S J, Zhang, Z, Li, X, Guo, C, Nisancioglu, K H, Stepanek, C, Lohmann, G, Sohl, L E, Chandler, M A, Tan, N, Contoux, C, Ramstein, G, Baatsen, M L J, Von Der Heydt, A S, Chandan, D, Peltier, W R, Abe-Ouchi, A, Chan, W L, Kamae, Y, Williams, C J R, Lunt, D J, Feng, R, Otto-Bliesner, B L & Brady, E C 2021, ' Mid-Pliocene West African Monsoon rainfall as simulated in the PlioMIP2 ensemble ', Climate of the Past, vol. 17, no. 4, pp. 1777-1794 . https://doi.org/10.5194/cp-17-1777-2021
Climate of the Past, 2021, 17 (4), pp.1777-1794. ⟨10.5194/cp-17-1777-2021⟩
The mid-Pliocene warm period (mPWP; ∼3.2 million years ago) is seen as the most recent time period characterized by a warm climate state, with similar to modern geography and ∼400 ppmv atmospheric CO2 concentration, and is therefore often conside
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::6d417484fe50bad519de17bfe7a0e0e2
https://hal.archives-ouvertes.fr/hal-03330098
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3
Evaluating the large-scale hydrological cycle response within the Pliocene Model Intercomparison Project Phase 2 (PlioMIP2) ensemble
Autor: Han, Z, Zhang, Q, Li, Q, Feng, R, Haywood, AM, Tindall, JC, Hunter, SJ, Otto-Bliesner, BL, Brady, EC, Rosenbloom, N, Zhang, Z, Li, X, Guo, C, Nisancioglu, KH, Stepanek, C, Lohmann, G, Sohl, LE, Chandler, MA, Tan, N, Ramstein, G, Baatsen, MLJ, von der Heydt, AS, Chandan, D, Peltier, WR, Williams, CJR, Lunt, DJ, Cheng, J, Wen, Q, Burls, NJ
Publikováno v: Climate of the Past
Climate of the Past, European Geosciences Union (EGU), 2021, 17 (6), pp.2537-2558. ⟨10.5194/cp-17-2537-2021⟩
Climate of the Past, 2021, 17 (6), pp.2537-2558. ⟨10.5194/cp-17-2537-2021⟩
Han, Z, Zhang, Q, Li, Q, Feng, R, Haywood, A M, Tindall, J C, Hunter, S J, Otto-Bliesner, B L, Brady, E C, Rosenbloom, N, Zhang, Z, Li, X, Guo, C, Nisancioglu, K H, Stepanek, C, Lohmann, G, Sohl, L E, Chandler, M A, Tan, N, Ramstein, G, Baatsen, M L J, Von Der Heydt, A S, Chandan, D, Peltier, W R, Williams, C J R, Lunt, D J, Cheng, J, Wen, Q & Burls, N J 2021, ' Evaluating the large-scale hydrological cycle response within the Pliocene Model Intercomparison Project Phase 2 (PlioMIP2) ensemble ', Climate of the Past, vol. 17, no. 6, pp. 2537-2558 . https://doi.org/10.5194/cp-17-2537-2021
International audience; Abstract. The mid-Pliocene (∼3 Ma) is one of the most recent warm periods with high CO2 concentrations in the atmosphere and resulting high temperatures, and it is often cited as an analog for near-term future climate change
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::00480606365cf2df4464d9d91d61f7b6
http://hdl.handle.net/10852/92882
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7
Modelled ocean changes at the Plio-Pleistocene transition driven by Antarctic ice advance
Autor: Hill, DJ, Bolton, KP, Haywood, AM
Publikováno v: Nature Communications, Vol 8, Iss 1, Pp 1-8 (2017)
The Earth underwent a major transition from the warm climates of the Pliocene to the Pleistocene ice ages between 3.2 and 2.6 million years ago. The intensification of Northern Hemisphere Glaciation is the most obvious result of the Plio-Pleistocene
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::a1c943f68e906eacb48b029f33ff482e
https://doaj.org/article/2587fadd10274af0beb6019ae4400086
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8
Akademický článek
Alpine permafrost could account for a quarter of thawed carbon based on Plio-Pleistocene paleoclimate analogue.
Autor: Cheng F; Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University, Beijing, 100871, China. cfcf.chengfeng@gmail.com.; Department of Earth and Environmental Sciences, University of Rochester, Rochester, NY, 14627, USA. cfcf.chengfeng@gmail.com., Garzione C; Department of Earth and Environmental Sciences, University of Rochester, Rochester, NY, 14627, USA.; Department of Environmental Sciences, Rochester Institute of Technology, Rochester, NY, 14623, USA.; College of Science, University of Arizona, Tucson, AZ, 85721, USA., Li X; Yunnan Key Laboratory of Earth System Science, Yunnan University, Kunming, 650500, China.; State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Science, Xi'an, 710061, China., Salzmann U; Department of Geography and Environmental Sciences, Northumbria University, Newcastle upon Tyne, NE1 8ST, UK., Schwarz F; Department of Geography and Environmental Sciences, Northumbria University, Newcastle upon Tyne, NE1 8ST, UK., Haywood AM; School of Earth and Environment, University of Leeds, Woodhouse Lane, Leeds, LS2 9JT, UK., Tindall J; School of Earth and Environment, University of Leeds, Woodhouse Lane, Leeds, LS2 9JT, UK., Nie J; Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou, 730000, China., Li L; College of Science, University of Arizona, Tucson, AZ, 85721, USA., Wang L; Department of Civil and Environmental Engineering, The Hong Kong University of Science and Technology, Hong Kong SAR, China., Abbott BW; Department of Plant and Wildlife Sciences, Brigham Young University, Provo, UT, USA., Elliott B; Department of Earth, Planetary, and Space Sciences, Department of Atmospheric and Oceanic Sciences, Institute of the Environment and Sustainability, Center for Diverse Leadership in Science, University of California, Los Angeles, CA, 90095, USA., Liu W; State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Science, Xi'an, 710061, China., Upadhyay D; Department of Earth, Planetary, and Space Sciences, Department of Atmospheric and Oceanic Sciences, Institute of the Environment and Sustainability, Center for Diverse Leadership in Science, University of California, Los Angeles, CA, 90095, USA., Arnold A; Department of Earth, Planetary, and Space Sciences, Department of Atmospheric and Oceanic Sciences, Institute of the Environment and Sustainability, Center for Diverse Leadership in Science, University of California, Los Angeles, CA, 90095, USA., Tripati A; Department of Earth, Planetary, and Space Sciences, Department of Atmospheric and Oceanic Sciences, Institute of the Environment and Sustainability, Center for Diverse Leadership in Science, University of California, Los Angeles, CA, 90095, USA.
Publikováno v: Nature communications [Nat Commun] 2022 Mar 14; Vol. 13 (1), pp. 1329. Date of Electronic Publication: 2022 Mar 14.
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9
Akademický článek
Past terrestrial hydroclimate sensitivity controlled by Earth system feedbacks.
Autor: Feng R; Department of Geosciences, College of Liberal Arts and Sciences, University of Connecticut, Mansfield, CT, USA. ran.feng@uconn.edu., Bhattacharya T; Department of Earth and Environmental Sciences, Syracuse University, Syracuse, NY, USA., Otto-Bliesner BL; Climate and Global Dynamics Laboratory, National Center for Atmospheric Research, Boulder, CO, USA., Brady EC; Climate and Global Dynamics Laboratory, National Center for Atmospheric Research, Boulder, CO, USA., Haywood AM; School of Earth and Environment, University of Leeds, Woodhouse Lane, Leeds, West Yorkshire, LS29JT, UK., Tindall JC; School of Earth and Environment, University of Leeds, Woodhouse Lane, Leeds, West Yorkshire, LS29JT, UK., Hunter SJ; School of Earth and Environment, University of Leeds, Woodhouse Lane, Leeds, West Yorkshire, LS29JT, UK., Abe-Ouchi A; Atmosphere and Ocean Research Institute, University of Tokyo, Kashiwa, Japan., Chan WL; Atmosphere and Ocean Research Institute, University of Tokyo, Kashiwa, Japan., Kageyama M; Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, F-91191, Gif-sur-Yvette, France., Contoux C; Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, F-91191, Gif-sur-Yvette, France., Guo C; NORCE Norwegian Research Centre, Bjerknes Centre for Climate Research, 5007, Bergen, Norway., Li X; Department of Atmospheric Science, School of Environnemental Studies, China University of Geoscience, Wuhan, 430074, China., Lohmann G; Alfred Wegener Institute-Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany.; University of Bremen, Bremen, Germany., Stepanek C; Alfred Wegener Institute-Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany., Tan N; Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China., Zhang Q; Department of Physical Geography and Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden., Zhang Z; Department of Atmospheric Science, School of Environnemental Studies, China University of Geoscience, Wuhan, 430074, China., Han Z; College of Oceanography, Hohai University, Nanjing, China., Williams CJR; School of Geographical Sciences and Cabot Institute, University of Bristol, University Road, Bristol, BS8 1SS, UK., Lunt DJ; School of Geographical Sciences and Cabot Institute, University of Bristol, University Road, Bristol, BS8 1SS, UK., Dowsett HJ; Florence Bascom Geoscience Center, U. S. Geological Survey, Reston, VA, USA., Chandan D; Department of Physics, University of Toronto, Toronto, CA, Canada., Peltier WR; Department of Physics, University of Toronto, Toronto, CA, Canada.
Publikováno v: Nature communications [Nat Commun] 2022 Mar 14; Vol. 13 (1), pp. 1306. Date of Electronic Publication: 2022 Mar 14.
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10
The Transient Response of Ice Volume to Orbital Forcing During the Warm Late Pliocene
Autor: De Boer, B, Haywood, AM, Dolan, AM, Hunter, SJ, Prescott, CL
Publikováno v: de Boer, B, Haywood, A M, Dolan, A M, Hunter, S J & Prescott, C L 2017, ' The Transient Response of Ice Volume to Orbital Forcing During the Warm Late Pliocene ', Geophysical Research Letters, vol. 44, no. 20, pp. 10,486-10,494 . https://doi.org/10.1002/2017GL073535
Geophysical Research Letters, 44(20), 10,486-10,494. American Geophysical Union
Examining the nature of ice sheet and sea level response to past episodes of enhanced greenhouse gas forcing may help constrain future sea level change. Here, for the first time, we present the transient nature of ice sheets and sea level during the
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::7a7f6c0d8ee02ee619615d43c19fab03
https://research.vu.nl/en/publications/2adfa8b4-90a8-474d-9cd1-2fa1682169ad
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