Remote sensing of surface albedo and cloud properties in the Arctic from AVHRR measurements

Dissertation (Ph.D.) University of Alaska Fairbanks, 1996 Based on a comprehensive radiative transfer model, algorithms suitable for arctic conditions are developed to retrieve broadband surface albedo and water cloud properties from National Oceanic and Atmospheric Administration (NOAA) Advanced Ve...

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Bibliographic Details
Main Author: Han, Wei
Other Authors: Stamnes, Knut, Bowling, Sue Ann, Harrison, William, Li, Shusun, Lubin, Dan, Watkins, Brenton
Format: Doctoral or Postdoctoral Thesis
Language:unknown
Published: 1996
Subjects:
Online Access:http://hdl.handle.net/11122/9426
id ftunivalaska:oai:scholarworks.alaska.edu:11122/9426
record_format openpolar
spelling ftunivalaska:oai:scholarworks.alaska.edu:11122/9426 2023-05-15T13:10:26+02:00 Remote sensing of surface albedo and cloud properties in the Arctic from AVHRR measurements Han, Wei Stamnes, Knut Bowling, Sue Ann Harrison, William Li, Shusun Lubin, Dan Watkins, Brenton 1996 http://hdl.handle.net/11122/9426 unknown http://hdl.handle.net/11122/9426 Physics Department Physics Atmospheric Science Remote sensing Dissertation phd 1996 ftunivalaska 2023-02-23T21:37:16Z Dissertation (Ph.D.) University of Alaska Fairbanks, 1996 Based on a comprehensive radiative transfer model, algorithms suitable for arctic conditions are developed to retrieve broadband surface albedo and water cloud properties from National Oceanic and Atmospheric Administration (NOAA) Advanced Very High Resolution Radiometer (AVHRR) narrowband measurements. Reflectance anisotropy of snow surfaces is first simulated by an discrete ordinates radiative transfer formulation, and is then included in the comprehensive model for the retrieval. Ground-based irradiance measurements made by NOAA Climate Monitoring and Diagnostics Laboratory (CMDL) in Barrow, Alaska are compared with retrieved albedo and downwelling irradiances computed from retrieved cloud optical depth and effective radius. Good agreement is found between satellite estimates and ground-based measurements, which indicate that the retrieval algorithms proposed in this thesis are suitable for arctic conditions. It is found that the effects of snow bidirectional reflectance on the retrieval of the broadband albedo are significant, and that the Lambertian approximation could lead to a 30% underestimate of the surface albedo. It is also found that cloud effective radius in the Arctic is generally smaller as compared with mid- and low-latitudes. Doctoral or Postdoctoral Thesis albedo Arctic Barrow Alaska University of Alaska: ScholarWorks@UA Arctic Fairbanks
institution Open Polar
collection University of Alaska: ScholarWorks@UA
op_collection_id ftunivalaska
language unknown
topic Physics
Atmospheric Science
Remote sensing
spellingShingle Physics
Atmospheric Science
Remote sensing
Han, Wei
Remote sensing of surface albedo and cloud properties in the Arctic from AVHRR measurements
topic_facet Physics
Atmospheric Science
Remote sensing
description Dissertation (Ph.D.) University of Alaska Fairbanks, 1996 Based on a comprehensive radiative transfer model, algorithms suitable for arctic conditions are developed to retrieve broadband surface albedo and water cloud properties from National Oceanic and Atmospheric Administration (NOAA) Advanced Very High Resolution Radiometer (AVHRR) narrowband measurements. Reflectance anisotropy of snow surfaces is first simulated by an discrete ordinates radiative transfer formulation, and is then included in the comprehensive model for the retrieval. Ground-based irradiance measurements made by NOAA Climate Monitoring and Diagnostics Laboratory (CMDL) in Barrow, Alaska are compared with retrieved albedo and downwelling irradiances computed from retrieved cloud optical depth and effective radius. Good agreement is found between satellite estimates and ground-based measurements, which indicate that the retrieval algorithms proposed in this thesis are suitable for arctic conditions. It is found that the effects of snow bidirectional reflectance on the retrieval of the broadband albedo are significant, and that the Lambertian approximation could lead to a 30% underestimate of the surface albedo. It is also found that cloud effective radius in the Arctic is generally smaller as compared with mid- and low-latitudes.
author2 Stamnes, Knut
Bowling, Sue Ann
Harrison, William
Li, Shusun
Lubin, Dan
Watkins, Brenton
format Doctoral or Postdoctoral Thesis
author Han, Wei
author_facet Han, Wei
author_sort Han, Wei
title Remote sensing of surface albedo and cloud properties in the Arctic from AVHRR measurements
title_short Remote sensing of surface albedo and cloud properties in the Arctic from AVHRR measurements
title_full Remote sensing of surface albedo and cloud properties in the Arctic from AVHRR measurements
title_fullStr Remote sensing of surface albedo and cloud properties in the Arctic from AVHRR measurements
title_full_unstemmed Remote sensing of surface albedo and cloud properties in the Arctic from AVHRR measurements
title_sort remote sensing of surface albedo and cloud properties in the arctic from avhrr measurements
publishDate 1996
url http://hdl.handle.net/11122/9426
geographic Arctic
Fairbanks
geographic_facet Arctic
Fairbanks
genre albedo
Arctic
Barrow
Alaska
genre_facet albedo
Arctic
Barrow
Alaska
op_relation http://hdl.handle.net/11122/9426
Physics Department
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