يعرض 1 - 10 نتائج من 81 نتيجة بحث عن '"Haywood, AM"', وقت الاستعلام: 1.63s تنقيح النتائج
  1. 1
  2. 2

    المساهمون: Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] (LSCE), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Sub Dynamics Meteorology, Sub Physical Oceanography, Marine and Atmospheric Research, Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)

    المصدر: 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⟩

    وصف الملف: application/pdf

  3. 3

    المساهمون: Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] (LSCE), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Modélisation du climat (CLIM), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Sub Dynamics Meteorology, Sub Physical Oceanography, Marine and Atmospheric Research, Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS), This research has been supported by the Swedish Research Council (Vetenskapsrådet, grant nos. 2013- 06476 and 2017-04232). The article processing charges for this open-access publication were covered by Stockholm University, Zixuan Han acknowledges financial support from the National Natural Science Foundation of China (grant no. 42130610), the Fundamental Research Funds for the Central Universities (grant no. B210201009), and the National Key R&D Program of China (grant no. 2017YFC1502303). Jianbo Cheng acknowledges financial support from the National Natural Science Foundation of China (grant no. 42005012) and the Natural Science Foundation of Jiangsu Province (grant no. BK20201058). Qin Wen acknowledges financial support from the National Natural Science Foundation of China (grant no. 42106016) and a project funded by the China Postdoctoral Science Foundation (grant no. 2021M691623). The EC-Earth3 model simulations and the data analysis were performed using the ECMWF computing and archive facilities and the Swedish National Infrastructure for Computing (SNIC) at the National Supercomputer Centre (NSC), which is partially funded by the Swedish Research Council through grant agreement no. 2018-05973. Charles J. R. Williams acknowledges financial support from the UK Natural Environment Research Council within the framework of the SWEET (Super-Warm Early Eocene Temperatures) project (grant no. NE/P01903X/1). Natalie J. Burls acknowledges support from the National Science Foundation (NSF, grant nos. AGS-1844380 and OCN-2002448) and the Alfred P. Sloan Foundation (as a research fellow). Ran Feng acknowledges sponsorship from the U.S. National Science Foundation (grant nos. 1903650 and 1814029). The contributions of Bette L. Otto-Bliesner, Esther C. Brady, and Nan Rosenbloom are based upon work supported by the National Center for Atmospheric Research, which is a major facility sponsored by the NSF under cooperative agreement no. 1852977. The CESM project is primarily supported by the National Science Foundation (NSF). Computing and data storage resources for the CESM and CCSM4 simulations, including the Cheyenne supercomputer (https://doi.org/10.5065/D6RX99HX), were provided by the Computational and Information Systems Laboratory (CISL) at NCAR. Xiangyu Li acknowledges financial support from the National Natural Science Foundation of China (NSFC, grant no. 42005042) and the China Scholarship Council (grant no. 201804910023). The NorESM simulations benefitted from resources provided by UNINETT Sigma2 – the national infrastructure for high-performance computing and data storage in Norway. The work by Anna S. von der Heydt and Michiel L. J. Baatsen was carried out in the framework of the Netherlands Earth System Science Centre (NESSC) program, which is financially supported by the Ministry of Education, Culture and Science (OCW grant no. 024.002.001). Simulations with CCSM4-Utrecht were performed at the SURFsara Dutch national computing facilities and were sponsored by NWO-EW (Netherlands Organisation for Scientific Research, Exact Sciences, project nos. 17189 and 2020.022). Christian Stepanek and Gerrit Lohmann acknowledge computational resources from the Computing and Data Centre of the Alfred Wegener Institute, Helmholtz-Zentrum für Polar- und Meeresforschung. Christian Stepanek and Gerrit Lohmann also acknowledge funding from the Helmholtz Climate Initiative REKLIM and the Alfred Wegener Institute's 'Changing Earth-Sustaining our Future' research program. The PRISM4 reconstruction and boundary conditions used in PlioMIP2 were funded by the U.S. Geological Survey Climate and Land Use Change Research and Development Program. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the US Government.

    المصدر: 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

    وصف الملف: application/pdf

  4. 4
  5. 5
  6. 6
  7. 7
  8. 8

    المساهمون: Sub Dynamics Meteorology, Marine and Atmospheric Research, Earth and Climate

    المصدر: 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

    وصف الملف: image/pdf; application/pdf

  9. 9
  10. 10