Regional aerosol warming enhanced by the diurnal cycle of low cloud

The datasets and codes contained here are for the paper with the information below. Questions or requests for additional information should be directed to the corresponding author with the email below. Ian Chang1,2, Lan Gao2, Adeyemi A. Adebiyi3, Sarah J. Doherty4,5, David Painemal6, William L. Smith Jr.6, Emily D. Lenhardt2, Abdulamid A. Fakoya2, Connor J. Flynn2, Jianyu Zheng7,8, Zhifeng Yang9, Patricia Castellanos8, Arlindo M. da Silva8, Zhibo Zhang7,10, Robert Wood5, Paquita Zuidema11, Sundar A. Christopher12, Jens Redemann2 1Department of Earth, Environmental, and Geographical Sciences, University of North Carolina at Charlotte, Charlotte, North Carolina, USA2School of Meteorology, University of Oklahoma, Norman, Oklahoma, USA3Department of Life and Environmental Sciences, University of California, Merced, Merced, California, USA4Cooperative Institute for Climate, Ocean and Ecosystem Studies, University of Washington, Seattle, Washington, USA5Department of Atmospheric and Climate Science, University of Washington, Seattle, Washington, USA6NASA Langley Research Center, Hampton, Virginia, USA7Goddard Earth Sciences Technology and Research II, University of Maryland Baltimore County, Baltimore, MD, USA8NASA Goddard Space Flight Center, Greenbelt, Maryland, USA9Graduate School, Howard University, Washington, District of Columbia, USA10Department of Physics, University of Maryland, Baltimore County, Baltimore, Maryland, USA11Rosenstiel School of Marine, Atmospheric, and Earth Science, University of Miami, Miami, Florida, USA12Department of Atmospheric and Earth Science, University of Alabama in Huntsville, Huntsville, Alabama, USA