海からの放射の大気散乱光に及ぼす影響の新しい計算法

• 高島 勉

  気象研究所

書誌事項

タイトル別名

• A new approach to evaluation of the atmospheric effects on upwelling radiance from the ocean.

抄録

   The reflection matrix of radiation just above the ocean surface is derived in a form suitable for the use of adding method. The air-water interface is separated by a ruffled surface, whose angular dependent reflection and transmission properties are calculated based on a Gaussian distribution of wave slopes (Cox and Munk, 1956). At present, the ocean is assumed to be vertically inhomogeneous, and its bottom to absorb all incident radiation. Polarization is included in the derivation of the equation. The reflection matrix of radiation thus derived enables us the computations of space radiance at the top of the atmosphere. The tiresome computation due to the polarity effect of radiation is overcome by the present method. Finally a sample computation is carried out in a scalar form.

収録刊行物

• 気象研究所研究報告

  気象研究所研究報告 34 (2), 75-81, 1983

  気象庁気象研究所

キーワード

• Atmospheric Science
• Geophysics

詳細情報

• CRID: 1390282681435531520
• NII論文ID: 130004484797
• DOI: 10.2467/mripapers.34.75
• ISSN: 18806643
• ISSN: 0031126X
• 本文言語コード: en
• データソース種別:
  • JaLC
  • Crossref
  • CiNii Articles
• 抄録ライセンスフラグ: 使用不可