Zobrazeno 1 - 10
of 18
pro vyhledávání: '"Tindall JC"'
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
Warmer than present Antarctic and Southern Ocean temperatures during the last interglacial, approximately 128,000 years ago, have been attributed to changes in north‐south ocean heat transport, causing opposing hemispheric temperature anomalies. We
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::0ba7fe70e89f4b26ed1d779f356ba3b2
https://eprints.whiterose.ac.uk/140055/7/Holloway_et_al-2018-Geophysical_Research_Letters.pdf
https://eprints.whiterose.ac.uk/140055/7/Holloway_et_al-2018-Geophysical_Research_Letters.pdf
Last Interglacial (LIG), stable water isotope values (δ¹⁸O) measured in Greenland deep ice cores are at least 2.5‰ higher compared to the present day. Previous isotopic climate simulations of the LIG do not capture the observed Greenland δ¹
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::dcd51aa7bc9d855cfa3438231bf6634f
https://eprints.whiterose.ac.uk/136028/1/revised_QSR_paper_jun2018.pdf
https://eprints.whiterose.ac.uk/136028/1/revised_QSR_paper_jun2018.pdf
Autor:
Pattnayak, KC, Gloor, E, Tindall, JC, Brienen, RJW, Barichivich, J, Baker, JCA, Spracklen, DV, Cintra, BBL, Coelho, CAS
São Paulo, Brazil has experienced severe water shortages and record low levels of its water reservoirs in 2013–2014. We evaluate the contributions of Amazon deforestation and climate change to low precipitation levels using a modelling approach, a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::6933e71f8ee1e2fefea3e35616a983d8
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