4.5 Article

Greenhouse- and orbital-forced climate extremes during the early Eocene

Publisher

ROYAL SOC
DOI: 10.1098/rsta.2017.0085

Keywords

climate change; Palaeocene-Eocene Thermal Maximum; hydrological cycle

Funding

  1. Heising-Simons Foundation
  2. National Science Foundation

Ask authors/readers for more resources

The Palaeocene-Eocene Thermal Maximum (PETM) was a significant global warming event in Earth's deep past (56 Mya). The warming across the PETM boundary was driven by a rapid rise in greenhouse gases. The event also coincided with a time of maximum insolation in Northern Hemisphere summer. There is increased evidence that the mean warming was accompanied by enhanced seasonality and/or extremes in precipitation (and flooding) and drought. A high horizontal resolution (50 km) global climate model is used to explore changes in the seasonal cycle of surface temperature, precipitation, evaporation minus precipitation and river run-off for regions where proxy data are available. Comparison for the regions indicates the model accurately simulates the observed changes in these climatic characteristics with North American interior warming and drying, and warming and increased river run-off at other regions. The addition of maximum insolation in Northern Hemisphere summer leads to a drier North America, but wetter conditions at most other locations. Long-range transport of atmospheric moisture plays a critical role in explaining regional changes in the water cycle. Such high-frequency variations in precipitation might also help explain discrepancies or misinterpretation of some climate proxies from the same locations, especially where sampling is coarse, i.e. at or greater than the frequency of precession. This article is part of a discussion meeting issue 'Hyperthermals: rapid and extreme global warming in our geological past'.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.5
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

Article Geochemistry & Geophysics

Large-scale, astronomically paced sediment input to the North Sea Basin during the Paleocene Eocene Thermal Maximum

Simin Jin, David B. Kemp, David W. Jolley, Manuel Vieira, James C. Zachos, Chunju Huang, Mingsong Li, Wenhan Chen

Summary: This study uncovers the impacts of extreme climate warming on sedimentary systems, revealing large-scale changes in sediment supply during the PETM and the importance of astronomical climate forcing in mediating these factors over long timescales.

EARTH AND PLANETARY SCIENCE LETTERS (2022)

Article Meteorology & Atmospheric Sciences

Increases in Future AR Count and Size: Overview of the ARTMIP Tier 2 CMIP5/6 Experiment

T. A. O'Brien, M. F. Wehner, A. E. Payne, C. A. Shields, J. J. Rutz, L-R Leung, F. M. Ralph, A. Collow, I Gorodetskaya, B. Guan, J. M. Lora, E. McClenny, K. M. Nardi, A. M. Ramos, R. Tome, C. Sarangi, E. J. Shearer, P. A. Ullrich, C. Zarzycki, B. Loring, H. Huang, H. A. Inda-Diaz, A. M. Rhoades, Y. Zhou

Summary: The ARTMIP project assesses the impact of uncertainties from AR detectors on our understanding of atmospheric rivers. The study compares AR statistics from CMIP5/6 simulations with reanalysis data and finds good agreement. Future simulations project an increase in AR frequency, counts, and sizes, especially along the western coastlines of the Pacific and Atlantic oceans. The choice of AR detector is the main contributor to the uncertainty in projected AR frequency.

JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES (2022)

Article Meteorology & Atmospheric Sciences

An Overview of ARTMIP's Tier 2 Reanalysis Intercomparison: Uncertainty in the Detection of Atmospheric Rivers and Their Associated Precipitation

A. B. Marquardt Collow, C. A. Shields, B. Guan, S. Kim, J. M. Lora, E. E. McClenny, K. Nardi, A. Payne, K. Reid, E. J. Shearer, R. Tome, J. D. Wille, A. M. Ramos, I. Gorodetskaya, L. R. Leung, T. A. O'Brien, F. M. Ralph, J. Rutz, P. A. Ullrich, M. Wehner

Summary: Atmospheric rivers play a crucial role in the hydrologic cycle by transporting water vapor poleward and causing precipitation, but their detection in large datasets still contains a lot of uncertainty. By comparing different algorithms and datasets, they found that the results of detection tools vary in different seasons and datasets.

JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES (2022)

Article Geosciences, Multidisciplinary

Global Changes in Terrestrial Vegetation and Continental Climate During the Paleocene-Eocene Thermal Maximum

Vera A. Korasidis, Scott L. Wing, Christine A. Shields, Jeffrey T. Kiehl

Summary: A compilation of terrestrial pollen and spores records across the Paleocene-Eocene transition at 38 sites globally revealed significant differences in PETM palynofloras compared to those in the late Paleocene or early Eocene post-PETM. Inferred paleoclimatic conditions indicated varying diversity of NLRs at different latitudes during the Paleocene and PETM periods.

PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY (2022)

Article Meteorology & Atmospheric Sciences

Atmospheric rivers impacting western North America in a world with climate intervention

Christine A. Shields, Jadwiga H. Richter, Angeline Pendergrass, Simone Tilmes

Summary: This study analyzes the impact of stratospheric aerosol injections on atmospheric rivers in western North America using simulations. The results show that without climate intervention, the atmospheric rivers will increase in southern California and decrease in the Pacific Northwest and coastal British Columbia by the end of the century. Moreover, the character of precipitation in the atmospheric rivers changes under climate engineering.

NPJ CLIMATE AND ATMOSPHERIC SCIENCE (2022)

Article Geosciences, Multidisciplinary

Evaluating Uncertainty and Modes of Variability for Antarctic Atmospheric Rivers

Christine A. Shields, Jonathan D. Wille, Allison B. Marquardt Collow, Michelle Maclennan, Irina Gorodetskaya

Summary: Atmospheric rivers (ARs) in Antarctica are influenced by synoptic environments and have varying impacts along coastlines and the continent. Detecting and defining ARs in Antarctica is challenging, but specific tools are effective in capturing ARs over inland ice sheets. Although different detection tools may yield inconsistent results, the large-scale synoptic environments and associated ARs show broad consistency. The western hemisphere of Antarctica is more connected to decadal and interannual modes of variability compared to the eastern hemisphere, and the influence of the Indian Ocean Dipole on Antarctic ARs is stronger when in phase with El Nino Southern Oscillation.

GEOPHYSICAL RESEARCH LETTERS (2022)

Article Geosciences, Multidisciplinary

Contribution of Atmospheric Rivers to Antarctic Precipitation

Michelle L. Maclennan, Jan T. M. Lenaerts, Christine Shields, Jonathan D. Wille

Summary: Atmospheric rivers are efficient mechanisms that transport atmospheric moisture from low latitudes to the Antarctic Ice Sheet. They contribute substantially to Antarctic precipitation, particularly in East Antarctica. They play an important role in the year-to-year variability of Antarctic precipitation and are crucial for understanding present and future trends in Antarctic mass balance.

GEOPHYSICAL RESEARCH LETTERS (2022)

Article Multidisciplinary Sciences

Astrochronology of the Paleocene-Eocene Thermal Maximum on the Atlantic Coastal Plain

Mingsong Li, Timothy J. Bralower, Lee R. Kump, Jean M. Self-Trail, James C. Zachos, William D. Rush, Marci M. Robinson

Summary: This study presents an astrochronology for the PETM carbon isotope excursion and suggests that astronomical forcing played a role in triggering the PETM event. The analysis of data from a paleoshelf environment indicates that the PETM onset lasted about 6 kyr and occurred during an extreme in precession. The study also supports the concept of carbonate saturation overshoot following global ocean acidification during the PETM.

NATURE COMMUNICATIONS (2022)

Article Geosciences, Multidisciplinary

Shelf Ecosystems Along the US Atlantic Coastal Plain Prior to and During the Paleocene-Eocene Thermal Maximum: Insights Into the Stratigraphic Architecture

Monika Doubrawa, Peter Stassen, Marci M. Robinson, Tali L. Babila, James C. Zachos, Robert P. Speijer

Summary: The Paleocene-Eocene Thermal Maximum (PETM) is a significant global warming event related to atmospheric CO2 increases during the early Paleogene. It is characterized by negative delta O-18 and delta C-13 excursions recorded in sedimentary archives and a disruption of the marine biosphere. This study focuses on the South Dover Bridge core in Maryland, which provides insights into the environmental changes and the transition from a well-oxygenated water column to a PETM-ecosystem under severe biotic stress-conditions.

PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY (2022)

Article Geochemistry & Geophysics

Sulfate and phosphate oxyanions alter B/Ca and d11B in inorganic calcite at constant pH: Crystallographic controls outweigh normal kinetic effects

Joji Uchikawa, Donald E. Penman, Dustin T. Harper, Jesse R. Farmer, James C. Zachos, Noah J. Planavsky, Richard E. Zeebe

Summary: We conducted inorganic experiments to investigate the effects of various oxyanions on the concentration and isotopic composition of boron in calcite. Sulfate and phosphate were found to have significant impacts on the incorporation of boron and isotopic fractionation during calcite precipitation. The observed kinetic trends of boron in the presence of sulfate and phosphate differ from previous studies, suggesting structural deformations of the calcite lattice due to the substitution of CO3. These findings have important implications for paleo-reconstructions of ocean chemistry.

GEOCHIMICA ET COSMOCHIMICA ACTA (2023)

Article Meteorology & Atmospheric Sciences

Characteristics and Variability of Winter Northern Pacific Atmospheric River Flavors

Yang Zhou, Travis A. O'Brien, William D. Collins, Christine A. Shields, Burlen Loring, Abdelrahman A. Elbashandy

Summary: Atmospheric rivers (ARs) are important for the global hydrological cycle and often associated with extreme weather events. This study categorizes winter North Pacific ARs into windy and wet ARs and compares their differences in lifecycle characteristics, overall frequency, landfall impacts, and variability.

JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES (2022)

Article Geosciences, Multidisciplinary

North Atlantic Drift Sediments Constrain Eocene Tidal Dissipation and the Evolution of the Earth-Moon System

David De Vleeschouwer, Donald E. E. Penman, Simon D'haenens, Fei Wu, Thomas Westerhold, Maximilian Vahlenkamp, Carlotta Cappelli, Claudia Agnini, Wendy E. C. Kordesch, Daniel J. J. King, Robin van der Ploeg, Heiko Palike, Sandra Kirtland Turner, Paul Wilson, Richard D. Norris, James C. C. Zachos, Steven M. M. Bohaty, Pincelli M. M. Hull

Summary: Cyclostratigraphy and astrochronology are important techniques in geologic timekeeping. The accuracy of astronomical calculations is crucial, but there are limitations due to solar system chaos. High-resolution paleoclimate records now allow for a reversal of the traditional approach, and the sediment records from Newfoundland Ridge are well-suited for this purpose.

PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY (2023)

Article Geosciences, Multidisciplinary

Future Atmospheric Rivers and Impacts on Precipitation: Overview of the ARTMIP Tier 2 High-Resolution Global Warming Experiment

Christine A. Shields, Ashley E. Payne, Eric Jay Shearer, Michael F. Wehner, Travis Allen O'Brien, Jonathan J. Rutz, L. Ruby Leung, F. Martin Ralph, Allison B. Marquardt Collow, Paul A. Ullrich, Qizhen Dong, Alexander Gershunov, Helen Griffith, Bin Guan, Juan Manuel Lora, Mengqian Lu, Elizabeth McClenny, Kyle M. Nardi, Mengxin Pan, Yun Qian, Alexandre M. Ramos, Tamara Shulgina, Maximiliano Viale, Chandan Sarangi, Ricardo Tome, Colin Zarzycki

Summary: Atmospheric rivers are important for Earth's hydrological cycle, delivering precipitation to local climates. The response of atmospheric rivers to climate change depends on how they are defined. Comparing 16 detection tools, it is found that atmospheric rivers generally increase in frequency and intensity, but the scale of the response varies depending on algorithmic criteria. The precipitation response to climate change is diverse and dependent on the chosen detection tools.

GEOPHYSICAL RESEARCH LETTERS (2023)

Article Meteorology & Atmospheric Sciences

Synoptic Drivers of Atmospheric River Induced Precipitation Near Dronning Maud Land, Antarctica

Rebecca Baiman, Andrew C. Winters, Jan Lenaerts, Christine A. Shields

Summary: Atmospheric rivers (ARs) can impact the Antarctic Ice Sheet (AIS) by transporting anomalous moisture from lower latitudes, which leads to extreme precipitation and increased radiation. They contribute significantly to the interannual variability of precipitation over the AIS, making them important for understanding future changes in the surface mass balance.

JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES (2023)

Article Meteorology & Atmospheric Sciences

Investigating Future Arctic Sea Ice Loss and Near-Surface Wind Speed Changes Related to Surface Roughness Using the Community Earth System Model

Alice K. DuVivier, Stephen J. Vavrus, Marika M. Holland, Laura Landrum, Christine A. Shields, Rudradutt Thaker

Summary: This study investigates the driving factors of wind trends in the Arctic, finding that changes in surface roughness and near-surface atmospheric stability are important contributors. Decreasing surface roughness leads to higher wind speeds and slower ice speeds. However, wind trends do not significantly impact Arctic sea ice loss.

JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES (2023)

No Data Available