Zobrazeno 1 - 10
of 31
pro vyhledávání: '"Heather L. Ford"'
Autor:
Yi Zhong, Ning Tan, Jordan T. Abell, Chijun Sun, Stefanie Kaboth-Bahr, Heather L. Ford, Timothy D. Herbert, Alex Pullen, Keiji Horikawa, Jimin Yu, Torben Struve, Michael E. Weber, Peter D. Clift, Juan C. Larrasoaña, Zhengyao Lu, Hu Yang, André Bahr, Tianyu Chen, Jingyu Zhang, Cao Wei, Wenyue Xia, Sheng Yang, Qingsong Liu
Publikováno v:
Nature Communications, Vol 15, Iss 1, Pp 1-10 (2024)
Abstract The investigation of triggers causing the onset and intensification of Northern Hemisphere Glaciation (NHG) during the late Pliocene is essential for understanding the global climate system, with important implications for projecting future
Externí odkaz:
https://doaj.org/article/b3df6bdd873d436095d75ccadf74aeb7
Autor:
Emily J. Judd, Jessica E. Tierney, Brian T. Huber, Scott L. Wing, Daniel J. Lunt, Heather L. Ford, Gordon N. Inglis, Erin L. McClymont, Charlotte L. O’Brien, Ronnakrit Rattanasriampaipong, Weimin Si, Matthew L. Staitis, Kaustubh Thirumalai, Eleni Anagnostou, Marlow Julius Cramwinckel, Robin R. Dawson, David Evans, William R. Gray, Ethan L. Grossman, Michael J. Henehan, Brittany N. Hupp, Kenneth G. MacLeod, Lauren K. O’Connor, Maria Luisa Sánchez Montes, Haijun Song, Yi Ge Zhang
Publikováno v:
Scientific Data, Vol 9, Iss 1, Pp 1-38 (2022)
Abstract Paleotemperature proxy data form the cornerstone of paleoclimate research and are integral to understanding the evolution of the Earth system across the Phanerozoic Eon. Here, we present PhanSST, a database containing over 150,000 data point
Externí odkaz:
https://doaj.org/article/eb7317ab4dfc4f0f8443ce579400f6ff
Publikováno v:
Nature Communications, Vol 9, Iss 1, Pp 1-6 (2018)
Speaking at a scientific conference helps spread scientific results and is also fundamental for career advancement. Here the authors show that at the American Geophysical Union Fall Meeting, the largest Earth and space science conference, women are o
Externí odkaz:
https://doaj.org/article/98523fe195d1435da73d77804504c638
Autor:
Noah J. Planavsky, Heather L Ford, Natalie J. Burls, Matthew D. Thomas, Pincelli M. Hull, Peter G. Jacobs, Donald E. Penman, Alexey V. Fedorov, Wei Liu, Madison Shankle
Publikováno v:
Nature
Nature, 2021, 598, pp.457-461. ⟨10.1038/s41586-021-03884-7⟩
Nature, 2021, 598, pp.457-461. ⟨10.1038/s41586-021-03884-7⟩
Ocean dynamics in the equatorial Pacific drive tropical climate patterns that affect marine and terrestrial ecosystems worldwide. How this region will respond to global warming has profound implications for global climate, economic stability and ecos
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::76e5caf60abd6525ba545215dd47ae9c
https://doi.org/10.1038/s41586-021-03884-7
https://doi.org/10.1038/s41586-021-03884-7
Autor:
Heather L. Ford, Natalie J. Burls, Peter Jacobs, Alexandra Jahn, Rocio P. Caballero-Gill, David A. Hodell, Alexey Fedorov
Geologic intervals of sustained warmth such as the mid-Pliocene warm period can inform our understanding of future climate change, including the long-term consequences of oceanic uptake of anthropogenic carbon. Here we generate carbon isotope records
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5c3f2accaa2bde91f72067c2201fe62b
https://doi.org/10.5194/egusphere-gc10-pliocene-17
https://doi.org/10.5194/egusphere-gc10-pliocene-17
Autor:
Heather L. Ford
For decades the mid-Pliocene warm period has been a data-model comparison target (PlioMIP, PlioVAR, PRISM). During the mid-Pliocene warm period (~3.2 Ma), global temperatures are estimated to be ~2.3°C warmer than today and atmospheric CO2 is estima
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ea34a99fdea0715c9894fdba8e57bf6e
https://doi.org/10.5194/egusphere-gc10-pliocene-66
https://doi.org/10.5194/egusphere-gc10-pliocene-66
Autor:
S. M. White, W. Richard Peltier, Melissa A. Berke, Wing-Le Chan, Anna von der Heydt, Kaustubh Thirumalai, Stijn De Schepper, Gerrit Lohmann, Deepak Chandan, Stephen J. Hunter, Molly O. Patterson, Chuncheng Guo, Erin L McClymont, Heather L Ford, Bjørg Risebrobakken, Alan M. Haywood, Ian Bailey, Julia Tindall, Carolien van der Weijst, Ran Feng, Francien Peterse, George E. A. Swann, Montserrat Alonso-Garcia, Bette L. Otto-Bliesner, Kate Littler, Michiel Baatsen, Esther C. Brady, Zhongshi Zhang, Kerim H. Nisancioglu, Benjamin Petrick, Ayako Abe-Ouchi, Jessica E. Tierney, Christian Stepanek, Sze Ling Ho, A. Christina Ravelo, Xiangyi Li
Publikováno v:
Climate of the Past. 16:1599-1615
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=doi_________::1f56c4121d8b7cd5df0fe7a8656b2623
https://doi.org/10.5194/cp-16-1599-2020
https://doi.org/10.5194/cp-16-1599-2020
Autor:
Heather L Ford, Maureen E. Raymo
Publikováno v:
Geology. 48:113-117
High-resolution seawater δ18O records, derived from coupled Mg/Ca and benthic δ18O analyses, can be used to evaluate how global ice volume changed during the mid-Pleistocene transition (MPT, ca. 1250–600 ka). However, such seawater δ18O records
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3253da86df507f2f204288c8eea1f1be
https://doi.org/10.1130/g46546.1
https://doi.org/10.1130/g46546.1
Autor:
Heather L Ford, A. Christina Ravelo
Publikováno v:
Paleoceanography and Paleoclimatology. 34:2-15
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::766acf702f7a9261b72b863dba44a690
https://doi.org/10.1029/2018pa003461
https://doi.org/10.1029/2018pa003461
Autor:
Matthew D. Thomas, Alexey V. Fedorov, Heather L Ford, Peter G. Jacobs, Natalie J. Burls, Pincelli M. Hull, Madison Shankle, Donald E. Penman, Noah J. Planavsky
The Pliocene epoch (5.3-2.6 million years ago) is the last time Earth experienced atmospheric carbon dioxide levels comparable to present day anthropogenic levels. As such, this time interval is a potential analogue for future, warmer Earth system st
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2487ea7aa9dc672818829e0ce191ef71
https://doi.org/10.5194/egusphere-egu21-680
https://doi.org/10.5194/egusphere-egu21-680