Mark J. Webb

发表

COSP: Satellite simulation software for model assessment

John M. Haynes, Robert Pincus, Stephen A. Klein, 2011 .

High cloud increase in a perturbed SST experiment with a global nonhydrostatic model including explicit convective processes

Shin-ichi Iga, Hirofumi Tomita, Masaki Satoh, 2014 .

Towards quantifying uncertainty in transient climate change

Matthew D. Collins, David M. H. Sexton, Mark J. Webb, 2006 .

Projected increase in continental runoff due to plant responses to increasing carbon dioxide

Olivier Boucher, David M. H. Sexton, Chris D. Jones, 2007, Nature.

Carbon dioxide induced stomatal closure increases radiative forcing via a rapid reduction in low cloud

Olivier Boucher, Jonathan M. Gregory, Marie Doutriaux-Boucher, 2009 .

Clearing clouds of uncertainty

Mark D. Zelinka, David A. Randall, Mark J. Webb, 2017 .

Accounting for Changing Temperature Patterns Increases Historical Estimates of Climate Sensitivity

Jonathan M. Gregory, Thorsten Mauritsen, Piers M. Forster, 2018, Geophysical Research Letters.

Frequency distributions of transient regional climate change from perturbed physics ensembles of general circulation model simulations

Matthew D. Collins, David M. H. Sexton, Mark J. Webb, 2006 .

Global mean cloud feedbacks in idealized climate change experiments

Johannes Quaas, Lawrence Buja, Monika Esch, 2006 .

The Cloud Feedback Model Intercomparison Project (CFMIP) contribution to CMIP6.

A. Pier Siebesma, Masahiro Watanabe, Bjorn Stevens, 2016 .

Mechanisms for the land/sea warming contrast exhibited by simulations of climate change

Jonathan M. Gregory, David M. H. Sexton, Manoj Joshi, 2008 .

An explanation for the difference between twentieth and twenty-first century land–sea warming ratio in climate models

Manoj Joshi, Mark J. Webb, M. Webb, 2013, Climate Dynamics.

A step-response approach for predicting and understanding non-linear precipitation changes

Jason Lowe, Peili Wu, Jonathan M. Gregory, 2012, Climate Dynamics.