Member Since 1999
Cathy L. Whitlock
Professor Emerita, Montana State University
AGU Research
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Earth Sciences Are the Model Sciences of the Anthropocene
PERSPECTIVES OF EARTH AND SPACE SCIENTISTS
21 september 2024
Daniel Richter, Sharon A. Billings, Susan L. Brant...

After 4.5 billion years as an evolving and dynamic planet, the Earth continues to evolve but with human‐altered dynamics. Earth scientists ha...

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A Link Between Hydroclimate Variability and Biomass Burning During the Last Millennium in the Interior Pacific Northwest
GEOPHYSICAL RESEARCH LETTERS
08 november 2023
Sam Mark, Mark B. Abbott, Byron A. Steinman, Aleja...

We present oxygen isotope and charcoal accumulation records from two lakes in eastern Washington that have sufficient temporal resolution to quanti...

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Hydroclimate and Biomass Burning in the Interior Pacific Northwest During the Medieval Climate Anomaly and Little Ice Age: Reconciling Different Proxy Archives
CLIMATE OF THE COMMON ERA II ORAL
paleoceanography and paleoclimatology | 15 december 2022
Sam Mark, Mark B. Abbott, Byron A. Steinman, Erika...
Climate change and its relationship to biomass burning over the past 1200 yr in northwestern North America remains a topic of open debate. Existing re...
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Quantifying black carbon emissions from lake sediments near late 13th century Māori settlements
THE PAST AND FUTURE OF FIRE: PALEO PERSPECTIVES, HISTORICAL UNDERSTANDING, AND FUTURE PROJECTIONS II ORAL
atmospheric sciences | 16 december 2021
Sandra Bruegger, David B. McWethy, Nathan Chellman...
Refractory black carbon (rBC) aerosols emitted from biomass and fossil fuel burning contribute to radiative forcing of climate. Understanding long-ter...
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Southern Westerlies and interannual climate variability as drivers of regional vegetation and fire history in southern South America (35-55°S)
CHANGES AND IMPACTS OF CLIMATE VARIABILITY IN SOUTH AMERICA I
global environmental change | 13 december 2019
William Nanavati, Cathy L. Whitlock, Virginia Igle...
Changes in fire activity and the position of the forest-steppe ecotone east of the Andes (35-55°S), inferred from a transect of pollen and charco...
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Hydrological changes in Yellowstone Lake (USA) during the Holocene based on the analysis of oxygen isotopes in diatoms
MAGMATIC AND HYDROTHERMAL ACTIVITY OF THE YELLOWSTONE PLATEAU, OR, HOW I LEARNED TO STOP WORRYING AND LOVE THE VOLCANO II
volcanology, geochemistry and petrology | 10 december 2019
Rosine Cartier, Daniel J. Conley, Melanie J. Leng,...
Northern Yellowstone Lake is on the southeast edge of the 631-ka Yellowstone caldera and is an area with high heat flow, high seismicity, and an abund...
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The HD-YLAKE project: or, How I Learned to Stop Worrying and Love the Smell of Hydrogen Sulfide
MAGMATIC AND HYDROTHERMAL ACTIVITY OF THE YELLOWSTONE PLATEAU, OR, HOW I LEARNED TO STOP WORRYING AND LOVE THE VOLCANO I
volcanology, geochemistry and petrology | 10 december 2019
Robert A. Sohn, Sherilyn C. Fritz, Robert N. Harri...
The Hydrothermal Dynamics of Yellowstone Lake (HD-YLAKE) project seeks to understand the cause-and-effect relationships among tectonic, magmatic, and ...
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THE DYNAMIC FLOOR OF YELLOWSTONE LAKE: A Geologic Record Over the Past 14 ka of Hydrothermal Explosions, Doming, and Faulting
MAGMATIC AND HYDROTHERMAL ACTIVITY OF THE YELLOWSTONE PLATEAU, OR, HOW I LEARNED TO STOP WORRYING AND LOVE THE VOLCANO II
volcanology, geochemistry and petrology | 10 december 2019
Lisa A. Morgan, Wayne C. Shanks, Nels A. Iverson, ...
Hydrothermal explosions represent a significant potential hazard in Yellowstone and particularly in Yellowstone Lake. The northern part of the lake is...
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