Zobrazeno 1 - 10
of 78
pro vyhledávání: '"Haywood AM"'
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:
McClymont, EL, Ford, HL, Ho, SL, Tindall, JC, Haywood, AM, Alonso-Garcia, M, Bailey, I, Berke, MA, Littler, K, Patterson, MO, Petrick, B, Peterse, F, Ravelo, AC, Risebrobakken, B, De Schepper, S, Swann, GEA, Thirumalai, K, Tierney, JE, van der Weijst, C, White, S, Abe-Ouchi, A, Baatsen, MLJ, Brady, EC, Chan, W-L, Chandan, D, Feng, R, Guo, C, von der Heydt, AS, Hunter, S, Li, X, Lohmann, G, Nisancioglu, KH, Otto-Bliesner, BL, Peltier, WR, Stepanek, C, Zhang, Z
Publikováno v:
Climate of the Past
1599–1615
1599–1615
A range of future climate scenarios are projected for high atmospheric CO2 concentrations, given uncertainties over future human actions as well as potential environmental and climatic feedbacks. The geological record offers an opportunity to underst
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::f79e79d788dae0ec37f55598ec2fd171
https://cp.copernicus.org/articles/16/1599/2020/
https://cp.copernicus.org/articles/16/1599/2020/
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
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
https://doaj.org/article/2587fadd10274af0beb6019ae4400086
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
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
https://research.vu.nl/en/publications/2adfa8b4-90a8-474d-9cd1-2fa1682169ad
The 8.2 ka event was a period of abrupt cooling of 1–3 °C across large parts of the Northern Hemisphere, which lasted for about 160 yr. The original hypothesis for the cause of this event has been the outburst of the proglacial Lakes Agassiz and O
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::52eb0f5fa3a8ed81cce70484ac6137fb
https://eprints.whiterose.ac.uk/117290/11/1-s2.0-S0012821X17303205-main.pdf
https://eprints.whiterose.ac.uk/117290/11/1-s2.0-S0012821X17303205-main.pdf
The El Niño Southern Oscillation (ENSO) drives interannual climate variability, hence its behavior over a range of climates needs to be understood. It is therefore important to verify that the paleoarchives, used for pre-instrumental ENSO studies, c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::4e7ca6069adf116e6284c625ee7d1761
https://eprints.whiterose.ac.uk/120121/1/Pliocene_isotopes_elnino_revised2.pdf
https://eprints.whiterose.ac.uk/120121/1/Pliocene_isotopes_elnino_revised2.pdf
Autor:
Tindall, JC, Haywood, AM
The first isotope-enabled general circulation model (GCM) simulations of the Pliocene are used to discuss the interpretation of δ18O measurements for a warm climate. The model suggests that spatial patterns of Pliocene ocean surface δ18O ( inline i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::573caabace73d85a232d3780984b8732
https://eprints.whiterose.ac.uk/90277/7/Tindall_et_al-2015-Paleoceanography.pdf
https://eprints.whiterose.ac.uk/90277/7/Tindall_et_al-2015-Paleoceanography.pdf