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Selecting global climate models for regional climate change studies

Proceedings of the National Academy of Sciences - PNAS, 2009-05, Vol.106 (21), p.8441-8446

2009

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Future dryness in the southwest US and the hydrology of the early 21st century drought

Proceedings of the National Academy of Sciences - PNAS, 2010-12, Vol.107 (50), p.21271-21276

2010

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Sustainable water deliveries from the Colorado River in a changing climate

Proceedings of the National Academy of Sciences - PNAS, 2009-05, Vol.106 (18), p.7334-7338

2009

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Human-Induced Changes in the Hydrology of the Western United States

Science (American Association for the Advancement of Science), 2008-02, Vol.319 (5866), p.1080-1083

2008

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The fingerprint of human-induced changes in the ocean's salinity and temperature fields

Geophysical research letters, 2012-11, Vol.39 (21), p.n/a

2012

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Attribution of Declining Western U.S. Snowpack to Human Effects

Journal of climate, 2008-12, Vol.21 (23), p.6425-6444

2008

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Detection and Attribution of Temperature Changes in the Mountainous Western United States

Journal of climate, 2008-12, Vol.21 (23), p.6404-6424

2008

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Detection of Anthropogenic Climate Change in the World's Oceans

Science (American Association for the Advancement of Science), 2001-04, Vol.292 (5515), p.270-274

2001

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Computed Tomographic Assessment of Individual Paranasal Sinus Compartment and Nasal Conchal Bulla Involvement in 300 Cases of Equine Sinonasal Disease

Frontiers in veterinary science, 2020-10, Vol.7, p.580356-580356

2020

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When will Lake Mead go dry?

Water resources research, 2008-03, Vol.44 (3), p.W03201-n/a

2008

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Anthropogenic Warming of the Oceans: Observations and Model Results

Journal of climate, 2006-05, Vol.19 (10), p.1873-1900

2006

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Three-dimensional tropospheric water vapor in coupled climate models compared with observations from the AIRS satellite system

Geophysical research letters, 2006-11, Vol.33 (21), p.L21701-n/a

2006

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Connections between the Pacific Ocean Tropics and Midlatitudes on Decadal Timescales

Journal of climate, 2000-03, Vol.13 (6), p.1173-1194

2000

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Interdecadal interactions between the tropics and midlatitudes in the Pacific Basin

Geophysical research letters, 1999-03, Vol.26 (5), p.615-618

1999

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Penetration of Human-Induced Warming into the World's Oceans

Science (American Association for the Advancement of Science), 2005-07, Vol.309 (5732), p.284-287

2005

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The Role of Climate Forecasts in Western U.S. Power Planning

Journal of applied meteorology and climatology, 2006-05, Vol.45 (5), p.653-673

2006

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Modeling of North Pacific Climate Variability Forced by Oceanic Heat Flux Anomalies

Journal of climate, 2001-10, Vol.14 (20), p.4027-4046

2001

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On the Roles of Tropical and Midlatitude SSTs in Forcing Interannual to Interdecadal Variability in the Winter Northern Hemisphere Circulation

Journal of climate, 1994-09, Vol.7 (9), p.1416-1441

1994

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Interdecadal Modulation of ENSO Teleconnections

Bulletin of the American Meteorological Society, 1998-12, Vol.79 (12), p.2715-2725

1998

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ENSO Influence on Intraseasonal Extreme Rainfall and Temperature Frequencies in the Contiguous United States: Observations and Model Results

Journal of climate, 1998-07, Vol.11 (7), p.1575-1586

1998

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Interdecadal variability of the Pacific Ocean: model response to observed heat flux and wind stress anomalies

Climate dynamics, 1994-03, Vol.9 (6), p.287-302

1994

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Ocean Circulations, Heat Budgets, and Future Commitment to Climate Change

Annual review of environment and resources, 2011-11, Vol.36 (1), p.27-43

2011

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Reply to comment by J. J. Barsugli et al. on “When will Lake Mead go dry?”

Water resources research, 2009-09, Vol.45 (9), p.W09602-n/a

2009

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Response of an atmospheric general circulation model to radiative forcing of tropical clouds

Journal of Geophysical Research - Atmospheres, 1994-10, Vol.99 (D10), p.20829-20845

1994

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The ACPI Project, Element 1: Initializing a Coupled Climate Model from Observed Conditions

Climatic change, 2004-01, Vol.62 (1-3), p.13-28

2004

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Selecting global climate models for regional climate change studies

Future dryness in the southwest US and the hydrology of the early 21st century drought

Sustainable water deliveries from the Colorado River in a changing climate

Human-Induced Changes in the Hydrology of the Western United States

The fingerprint of human-induced changes in the ocean's salinity and temperature fields

Attribution of Declining Western U.S. Snowpack to Human Effects

Detection and Attribution of Temperature Changes in the Mountainous Western United States

Detection of Anthropogenic Climate Change in the World's Oceans

Computed Tomographic Assessment of Individual Paranasal Sinus Compartment and Nasal Conchal Bulla Involvement in 300 Cases of Equine Sinonasal Disease

When will Lake Mead go dry?

Anthropogenic Warming of the Oceans: Observations and Model Results

Three-dimensional tropospheric water vapor in coupled climate models compared with observations from the AIRS satellite system

Connections between the Pacific Ocean Tropics and Midlatitudes on Decadal Timescales

Interdecadal interactions between the tropics and midlatitudes in the Pacific Basin

Penetration of Human-Induced Warming into the World's Oceans

The Role of Climate Forecasts in Western U.S. Power Planning

Modeling of North Pacific Climate Variability Forced by Oceanic Heat Flux Anomalies

On the Roles of Tropical and Midlatitude SSTs in Forcing Interannual to Interdecadal Variability in the Winter Northern Hemisphere Circulation

Interdecadal Modulation of ENSO Teleconnections

ENSO Influence on Intraseasonal Extreme Rainfall and Temperature Frequencies in the Contiguous United States: Observations and Model Results

Interdecadal variability of the Pacific Ocean: model response to observed heat flux and wind stress anomalies

Ocean Circulations, Heat Budgets, and Future Commitment to Climate Change

Reply to comment by J. J. Barsugli et al. on “When will Lake Mead go dry?”

Response of an atmospheric general circulation model to radiative forcing of tropical clouds

The ACPI Project, Element 1: Initializing a Coupled Climate Model from Observed Conditions

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