MESOSPHERIC TEMPERATURES FROM RAYLEIGH-SCATTERING MEASUREMENTS BY THE WINDII INSTRUMENT ON UARS

被引：8

作者：

EVANS, WFJ ^{[1
]}

LAFRAMBOISE, LR ^{[1
]}

SHEPHERD, GG ^{[1
]}

机构：

[1] YORK UNIV,CTR RES EARTH & SPACE SCI,N YORK M3J 1P3,ON,CANADA

来源：

EARTHS MIDDLE ATMOSPHERE | 1994年 / 14卷 / 09期

基金：

加拿大自然科学与工程研究理事会;

关键词：

D O I：

10.1016/0273-1177(94)90150-3

中图分类号：

V [航空、航天];

学科分类号：

08 ; 0825 ;

摘要：

The WINDII instrument on the UARS satellite has several filter channels. In each of these channels, Rayleigh scattering from the earth's atmosphere is measured in the daytime. The Rayleigh scattering component varies quasi-exponentially with altitude with the scale height of the atmosphere. This data first must be corrected for the relevant baffle scattering component. After several corrections, temperatures from about 75 to 110 km can be measured. The development of the algorithm is discussed and several typical temperature profiles are presented. An analysis of the errors and comparisons with current upper atmosphere models are considered. The presence of noctilucent clouds is indicated in several August profiles in the northern hemisphere.

引用

页码：285 / 288

页数：4

共 4 条

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[2]

BARNETT JJ, 1984, MAP HDB, V13

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