Modeled and empirical approaches for retrieving columnar water vapor from solar transmittance measurements in the 0.72, 0.82, and 0.94 mu m absorption bands
T. Ingold et al., Modeled and empirical approaches for retrieving columnar water vapor from solar transmittance measurements in the 0.72, 0.82, and 0.94 mu m absorption bands, J GEO RES-A, 105(D19), 2000, pp. 24327-24343
A Sun photometer (18 channels between 300 and 1024 nm) has been used for me
asuring the columnar content of atmospheric water vapor (CWV) by solar tran
smittance measurements in absorption bands with channels centered at 719, 8
17, and 946 nm. The observable is the band-weighted transmittance function
defined by the spectral absorption of water vapor and the spectral features
of solar irradiance and system response. The transmittance function is app
roximated by a three-parameter model. Its parameters are determined from MO
DTRAN and LBLRTM simulations or empirical approaches using CWV data of a du
al-channel microwave radiometer (MWR) or a Fourier transform spectrometer (
FTS). Data acquired over a 2-year period during 1996-1998 at two different
sites in Switzerland, Bern (560 m above sea level (asl)) and Jungfraujoch (
3580 m asl) were compared to MWR, radiosonde (RS), and FTS retrievals. At t
he low-altitude station with an average CWV amount of 15 mm the LBLRTM appr
oach (based on recently corrected line intensities) leads to negligible bia
ses at 719 and 946 nm if compared to an average of MWR, RS, and GPS retriev
als. However, at 817 nm an overestimate of 2.7 to 4.3 mm (18-29%) remains.
At the high-altitude station with an average CWV amount of 1.4 mm the LBLRT
M approaches overestimate the CWV by 1.0, 1.4, and 0.1 mm (58, 76, and 3%)
at 719, 817, and 946 nm, compared to the FTS instrument. At the low-altitud
e station, CWV estimates, based on empirical approaches, agree with the MWR
within 0.4 mm (2.5% of the mean); at the high-altitude site with a factor
of 10 less water vapor the agreement of the SPM with the FTS is 0.0 to 0.2
mm (1 to 9% of the mean CWV there). Sensitivity analyses show that for the
conditions met at the two stations with CWV ranging from 0.2 to 30 mm, the
retrieval errors are smallest if the 946 nm channel is used.