Search Results
. 1995 ; Wyant et al. 1997 ; Sandu and Stevens 2011 ; Van der Dussen et al. 2013 ; De Roode et al. 2016 ; Neggers et al. 2017 ) in an effort to identify key controls, such as inversion stability ( Klein and Hartmann 1993 ; Sandu and Stevens 2011 ), increasing latent heat fluxes over warmer SSTs ( Bretherton and Wyant 1997 ), subsidence ( Van der Dussen et al. 2016 ), free tropospheric humidity ( Klein et al. 1995 ; Sandu and Stevens 2011 ; Eastman and Wood 2018 ) and aerosol and its feedback
. 1995 ; Wyant et al. 1997 ; Sandu and Stevens 2011 ; Van der Dussen et al. 2013 ; De Roode et al. 2016 ; Neggers et al. 2017 ) in an effort to identify key controls, such as inversion stability ( Klein and Hartmann 1993 ; Sandu and Stevens 2011 ), increasing latent heat fluxes over warmer SSTs ( Bretherton and Wyant 1997 ), subsidence ( Van der Dussen et al. 2016 ), free tropospheric humidity ( Klein et al. 1995 ; Sandu and Stevens 2011 ; Eastman and Wood 2018 ) and aerosol and its feedback
reaching the inversion. Cloud-top entrainment profoundly impacts the type and coverage of clouds within the MBL because it plays such an important role in the MBL moisture, heat, and momentum budgets ( Lilly 1968 ; Bretherton and Wyant 1997 ; Wyant et al. 1997 ; Stevens 2002 ; Stevens et al. 2002 ). In addition, cloud-top entrainment controls how MBL clouds respond to increased greenhouse gases ( Caldwell and Bretherton 2009 ) and atmospheric aerosols ( Ackerman et al. 2004 ; Wood 2007
reaching the inversion. Cloud-top entrainment profoundly impacts the type and coverage of clouds within the MBL because it plays such an important role in the MBL moisture, heat, and momentum budgets ( Lilly 1968 ; Bretherton and Wyant 1997 ; Wyant et al. 1997 ; Stevens 2002 ; Stevens et al. 2002 ). In addition, cloud-top entrainment controls how MBL clouds respond to increased greenhouse gases ( Caldwell and Bretherton 2009 ) and atmospheric aerosols ( Ackerman et al. 2004 ; Wood 2007
