Diurnal Cycles of Clouds and How They Affect Polar-Orbiting Satellite Data

Abstract Diurnal cycles of clouds were investigated using the NOAA series of polar-orbiting satellites. These satellites provided four observations per day for a continuous 11-yr period from 1986 to 1997. The High Resolution Infrared Radiation Sounder (HIRS) multispectral infrared data were used from the time trend analysis of Wylie et al. The previous study restricted its discussion to only the polar orbiters making observations at 0200 and 1400 LT because gaps in coverage occurred in the 0800 and 2000 LT coverage. This study shows diurnal cycles in cloud cover over 10% in amplitude in many regions, which is very similar to other studies that used geostationary satellite data. The use of only one of the polar-orbiting satellites by Wylie et al. caused biases up to 5% in small regions but in general they were small (e.g., ≤2% for most of the earth). The only consistently large bias was in high cloud cover over land in North America, Europe, and Asia north of 35°N latitude in the summer season where the 02...

[1]  W. Menzel,et al.  Four Years of Global Cirrus Cloud Statistics Using HIRS, Revised , 1994 .

[2]  D. Jackson,et al.  Trends in Global Cloud Cover in Two Decades of HIRS Observations , 2005 .

[3]  W. M. Gray,et al.  Diurnal Variation of Deep Cumulus Convection , 1977 .

[4]  W. Menzel,et al.  Eight Years of High Cloud Statistics Using HIRS , 1999 .

[5]  Donald P. Wylie,et al.  The Diurnal Cycle of Upper-Tropospheric Clouds Measured by GOES-VAS and the ISCCP , 2002 .

[6]  Michael J. Pavolonis,et al.  Global Daytime Distribution of Overlapping Cirrus Cloud from NOAA’s Advanced Very High Resolution Radiometer , 2005 .

[7]  H. Hendon,et al.  The diurnal cycle of tropical convection , 1993 .

[8]  Claudia J. Stubenrauch,et al.  Clouds as Seen by Satellite Sounders (3I) and Imagers (ISCCP). Part I: Evaluation of Cloud Parameters , 1999 .

[9]  W. Rossow,et al.  Advances in understanding clouds from ISCCP , 1999 .

[10]  Lena Iredell,et al.  Characteristics of the TOVS Pathfinder Path A Dataset , 1997 .

[11]  J. Duvel Convection over Tropical Africa and the Atlantic Ocean during Northern Summer. Part I: Interannual and Diurnal Variations , 1989 .

[12]  A. Gruber,et al.  Diurnal variation of the ISCCP cloudiness , 1994 .

[13]  Claudia J. Stubenrauch,et al.  Clouds as Seen by Satellite Sounders (3I) and Imagers (ISCCP). Part III: Spatial Heterogeneity and Radiative Effects , 1999 .

[14]  Murry L. Salby,et al.  Diurnal Variations of Cloud Cover and Their Relationship to Climatological Conditions , 1996 .

[15]  Taneil Uttal,et al.  Daytime Global Cloud Typing from AVHRR and VIIRS: Algorithm Description, Validation, and Comparisons , 2005 .

[16]  A. Chédin,et al.  Clouds as Seen by Satellite Sounders (3I) and Imagers (ISCCP). Part II: A New Approach for Cloud Parameter Determination in the 3I Algorithms , 1999 .

[17]  Brian Cairns,et al.  Diurnal variations of cloud from ISCCP data , 1995 .

[18]  A. Betts,et al.  Convection in GATE , 1981 .

[19]  Donald P. Wylie,et al.  Comparison of the Climatologies of High-Level Clouds from HIRS and ISCCP , 1996 .

[20]  A. Gruber,et al.  Seasonal and annual variability of the diurnal cycle of clouds , 1996 .

[21]  Michael J. Pavolonis,et al.  Comparison of NOAA's Operational AVHRR-Derived Cloud Amount to Other Satellite-Derived Cloud Climatologies , 2004 .

[22]  Robert A. Houze,et al.  Diurnal variation and life‐cycle of deep convective systems over the tropical pacific warm pool , 1997 .