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Human-driven greenhouse gas and aerosol emissions cause distinct regional impacts on extreme fire weather

Nature communications, 2021-01, Vol.12 (1), p.212-8, Article 212

2021

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Are Glacials Dry? Consequences for Paleoclimatology and for Greenhouse Warming

Journal of climate, 2017-09, Vol.30 (17), p.6593-6609

2017

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Projected drought risk in 1.5°C and 2°C warmer climates

Geophysical research letters, 2017-07, Vol.44 (14), p.7419-7428

2017

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CO2-plant effects do not account for the gap between dryness indices and projected dryness impacts in CMIP6 or CMIP5

Environmental research letters, 2021-03, Vol.16 (3), p.034018

2021

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Stormquakes

Geophysical research letters, 2019-11, Vol.46 (22), p.12909-12918

2019

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Exacerbation of the 2013-2016 Pan-Caribbean Drought by Anthropogenic Warming

Geophysical research letters, 2018-10, Vol.45 (19), p.10,619-10,626

2018

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The Value of Initial Condition Large Ensembles to Robust Adaptation Decision‐Making

Earth's future, 2020-10, Vol.8 (10), p.n/a

2020

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California margin temperatures modulate regional circulation and extreme summer precipitation in the desert Southwest

Environmental research letters, 2023-10, Vol.18 (10), p.104048

2023

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North American megadroughts in the Common Era: reconstructions and simulations

Wiley interdisciplinary reviews. Climate change, 2016-05, Vol.7 (3), p.411-432

2016

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The improbable but unexceptional occurrence of megadrought clustering in the American West during the Medieval Climate Anomaly

Environmental research letters, 2016-07, Vol.11 (7), p.74025

2016

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Why do the Global Warming Responses of Land‐Surface Models and Climatic Dryness Metrics Disagree?

Earth's future, 2022-08, Vol.10 (8), p.n/a

2022

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Does Regional Hydroclimate Change Scale Linearly With Global Warming?

Geophysical research letters, 2021-12, Vol.48 (23), p.n/a

2021

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Atlantic‐Pacific Gradients Drive Last Millennium Hydroclimate Variability in Mesoamerica

Geophysical research letters, 2020-07, Vol.47 (13), p.n/a

2020

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Hydroclimate Dipole Drives Multi‐Centennial Variability in the Western Tropical North Atlantic Margin During the Middle and Late Holocene

Paleoceanography and paleoclimatology, 2021-07, Vol.36 (7), p.n/a

2021

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Global warming and 21st century drying

Climate dynamics, 2014-11, Vol.43 (9-10), p.2607-2627

2014

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Forced changes in the Pacific Walker circulation over the past millennium

Nature (London), 2023-10, Vol.622 (7981), p.93-100

2023

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Twenty-first century hydroclimate: A continually changing baseline, with more frequent extremes

Proceedings of the National Academy of Sciences - PNAS, 2022-03, Vol.119 (12), p.e2108124119-e2108124119

2022

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Imprint of the Pacific Walker Circulation in Global Precipitation δ18O

Journal of climate, 2021-11, Vol.34 (21), p.8579-8597

2021

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Imprint of the Pacific Walker Circulation in Global Precipitation δ18O

Journal of climate, 2021-11, Vol.34 (21), p.8579-8597

2021

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Understanding Diverse Model Projections of Future Extreme El Niño

Journal of climate, 2021-01, Vol.34 (2), p.449-464

2021

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Are Simulated Megadroughts in the North American Southwest Forced?

Journal of climate, 2015-01, Vol.28 (1), p.124-142

2015

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The challenge of accurately quantifying future megadrought risk in the American Southwest

Geophysical research letters, 2016-09, Vol.43 (17), p.9225-9233

2016

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CO 2 -plant effects do not account for the gap between dryness indices and projected dryness impacts in CMIP6 or CMIP5

Environmental research letters, 2021-03, Vol.16 (3), p.34018

2021

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Complex drivers of reef-fronted beach change

Marine geology, 2022-04, Vol.446, p.106770, Article 106770

2022

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Climate Variability, Volcanic Forcing, and Last Millennium Hydroclimate Extremes

Journal of climate, 2018-06, Vol.31 (11), p.4309-4327

2018

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Human-driven greenhouse gas and aerosol emissions cause distinct regional impacts on extreme fire weather

Are Glacials Dry? Consequences for Paleoclimatology and for Greenhouse Warming

Projected drought risk in 1.5°C and 2°C warmer climates

CO2-plant effects do not account for the gap between dryness indices and projected dryness impacts in CMIP6 or CMIP5

Stormquakes

Exacerbation of the 2013-2016 Pan-Caribbean Drought by Anthropogenic Warming

The Value of Initial Condition Large Ensembles to Robust Adaptation Decision‐Making

California margin temperatures modulate regional circulation and extreme summer precipitation in the desert Southwest

North American megadroughts in the Common Era: reconstructions and simulations

The improbable but unexceptional occurrence of megadrought clustering in the American West during the Medieval Climate Anomaly

Why do the Global Warming Responses of Land‐Surface Models and Climatic Dryness Metrics Disagree?

Does Regional Hydroclimate Change Scale Linearly With Global Warming?

Atlantic‐Pacific Gradients Drive Last Millennium Hydroclimate Variability in Mesoamerica

Hydroclimate Dipole Drives Multi‐Centennial Variability in the Western Tropical North Atlantic Margin During the Middle and Late Holocene

Global warming and 21st century drying

Forced changes in the Pacific Walker circulation over the past millennium

Twenty-first century hydroclimate: A continually changing baseline, with more frequent extremes

Imprint of the Pacific Walker Circulation in Global Precipitation δ18O

Imprint of the Pacific Walker Circulation in Global Precipitation δ18O

Understanding Diverse Model Projections of Future Extreme El Niño

Are Simulated Megadroughts in the North American Southwest Forced?

The challenge of accurately quantifying future megadrought risk in the American Southwest

CO 2 -plant effects do not account for the gap between dryness indices and projected dryness impacts in CMIP6 or CMIP5

Complex drivers of reef-fronted beach change

Climate Variability, Volcanic Forcing, and Last Millennium Hydroclimate Extremes

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