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Atmospheric remote sensing

Waters J W 1993 Miorowave limb sounding Atmospheric Remote Sensing by Microwave Radiometry ed M A Janssen (New York Wiley) pp 383-496... [Pg.1259]

Janssen M A (ed) 1993 Atmospheric Remote Sensing by Microwave Radiometry (New York Wiiey) The most oompiete guide to miorowave and THz atmospherio sensing. [Pg.1262]

One of the first examples of the modem application of remote sensing of the composition of the atmosphere was the assertion by Hartley in 1880 that the UV absorption in the solar absorption spectrum was attributable to ozone. In this manner the earth s stratospheric ozone layer was discovered. Since this pioneering work and especially in die past 30 years, there has been rapid progress in the development of atmospheric remote sensing techniques. [Pg.303]

In the next few years a number of important atmospheric remote sensing missions are planned by NASDA, NASA and ESA. NASDA has constructed a second ADEOS satellite which will have POLDER and ILAS-II (Improved Limb Atmospheric Sounder) on board. The NASA-TERRA platform was launched at the end of 1999 and has the MOPITT instrument (Measurement of Pollution in the Troposphere), which aims to measure vertical profiles of carbon monoxide and methane in the troposphere. MOPITT is a Canadian instrument supported by an international science team. [Pg.320]

Edwards, D.P., M. Lopez-Puertas, and M.A. Lopez-Valverde, Non-local thermodynamic equilibrium studies of the 15-jUm bands of CO2 for atmospheric remote sensing. J Geophys Res 98, 14,955, 1993. [Pg.253]

M. A. Janssen, ed., Atmospheric Remote Sensing by Microwave Radiomety, J ohn Wiley Sons, Inc., New York, 1993. [Pg.322]

Burrows, J. P., Richter, A., Dehn, A., Deters, B., Himmelmann, S., Voigt, S., and Orphal, J. (1999) Atmospheric remote sensing reference data from GOME—2. Temperature-dependent absorption cross sections of 03 in the 231-794 nm range, J. Quant. Spectros. Radiative Transf. 61, 509-517. [Pg.136]

In atmospheric remote-sensing applications, the statistical interpretation of constrained inversion often is associated with the studies by Strand and Westwater [15-16] and Rodgers [19] and the following formulations ... [Pg.75]

For constraining a retrieval by a priori estimates a as in Eqs. (33-35), one can use information about typical magnitudes and variabilities of the parameters a. For example, in atmospheric remote sensing applications. [Pg.84]

A. Asmann, R. Neuber, R Rairoux (eds.), Advances in Atmospheric Remote Sensing with LIDAR (Springer, Berlin, 1997)... [Pg.744]

M.M. Sokolski (ed.), Laser Applications in Meteorology and Earth- and Atmospheric Remote Sensing. SPIE Proc., vol. 1062 (1989)... [Pg.744]

Bogumil, K., Orphal, J., Homann, T., Voigt, S., Spietz, P., Fleischmaim, O.C., Vogel, A., Hartmann, M., Bovensmann, H., Frerick, J., Burrows, J.P. Measurements of molecular absorption spectra with the SCIAMACHY pre-flight model instrument characterization and reference data for atmospheric remote-sensing in the 230-2380 nm region. J. Photochem. Photobiol. A Chem. 157, 167-184 (2003)... [Pg.154]


See other pages where Atmospheric remote sensing is mentioned: [Pg.158]    [Pg.256]    [Pg.324]    [Pg.346]    [Pg.67]    [Pg.97]    [Pg.422]    [Pg.130]    [Pg.148]    [Pg.84]    [Pg.333]   
See also in sourсe #XX -- [ Pg.146 , Pg.188 , Pg.318 ]




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