Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Sohl LE"'
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⟩
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
https://hal.archives-ouvertes.fr/hal-03330098
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
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
http://hdl.handle.net/10852/92882
Autor:
Haywood, AM, Tindall, JC, Dowsett, HJ, Dolan, AM, Foley, KM, Hunter, SJ, Hill, DJ, Chan, W-L, Abe-Ouchi, A, Stepanek, C, Lohmann, G, Chandan, D, Peltier, WR, Tan, N, Contoux, C, Ramstein, G, Li, X, Zhang, Z, Guo, C, Nisancioglu, KH, Zhang, Q, Li, Q, Kamae, Y, Chandler, MA, Sohl, LE, Otto-Bliesner, BL, Feng, R, Brady, EC, Von der Heydt, AS, Baatsen, MLJ, Lunt, DJ
The Pliocene epoch has great potential to improve our understanding of the long-term climatic and environmental consequences of an atmospheric CO2 concentration near ~ 400 parts per million by volume. Here we present the large-scale features of Plioc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::dd872e855df89f7f25c77cb8c6206062
https://eprints.whiterose.ac.uk/155346/1/cp-2019-145.pdf
https://eprints.whiterose.ac.uk/155346/1/cp-2019-145.pdf
Autor:
Haywood, AM, Tindall, JC, Dowsett, HJ, Dolan, AM, Foley, KM, Hunter, SJ, Hill, DJ, Chan, W-L, Abe-Ouchi, A, Stepanek, C, Lohmann, G, Chandan, D, Peltier, WR, Tan, N, Contoux, C, Ramstein, G, Li, X, Zhang, Z, Guo, C, Nisancioglu, KH, Zhang, Q, Li, Q, Kamae, Y, Chandler, MA, Sohl, LE, Otto-Bliesner, BL, Feng, R, Brady, EC, Von der Heydt, AS, Baatsen, MLJ, Lunt, DJ, Sub Physical Oceanography, Sub Dynamics Meteorology, Marine and Atmospheric Research
Publikováno v:
Climate of the Past, 16, 2095. European Geosciences Union
The Pliocene epoch has great potential to improve our understanding of the long-term climatic and environmental 35 consequences of an atmospheric CO2 concentration near ~400 parts per million by volume. Here we present the large-scale features of Pli
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=narcis______::887727ec2ee75879cd76b0e60d0eb82e
https://dspace.library.uu.nl/handle/1874/408123
https://dspace.library.uu.nl/handle/1874/408123
Autor:
de Nooijer, W, Zhang, Q, Li, Q, Li, X, Zhang, Z, Guo, C, Nisancioglu, KH, Haywood, A, Tindall, J, Hunter, S, Dowsett, HJ, Stepanek, C, Lohmann, G, Otto-Bliesner, BL, Feng, R, Sohl, LE, Chandler, MA, Tan, N, Contoux, C, Ramstein, G, Baatsen, MLJ, von der Heydt, A, Chandan, D, Peltier, WR, Abe-Ouchi, A, Chan, W-L, Kamae, Y, Brierley, CM
Publikováno v:
Climate of the Past
Climate of the Past, 2020, 16 (6), pp.2325-2341. ⟨10.5194/cp-16-2325-2020⟩
Climate of the Past, European Geosciences Union (EGU), 2020, 16 (6), pp.2325-2341. ⟨10.5194/cp-16-2325-2020⟩
Climate of the Past, 2020, 16 (6), pp.2325-2341. ⟨10.5194/cp-16-2325-2020⟩
Climate of the Past, European Geosciences Union (EGU), 2020, 16 (6), pp.2325-2341. ⟨10.5194/cp-16-2325-2020⟩
Palaeoclimate simulations improve our understanding of the climate, inform us about the performance of climate models in a different climate scenario, and help to identify robust features of the climate system. Here, we analyse Arctic warming in an e
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::4778bf39615ae0d20bf56d429e458ed2
https://hal.science/hal-03053373
https://hal.science/hal-03053373
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.