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This study compares water vapor measurements taken using the AATS-14 and J31 in-situ instruments during ICARTT-2004. The calculations involve columnar water vapor density derived from AATS-14 data and the relative humidity determination using the Vaisala HMP243. The text highlights the methods and findings of the comparison between different measurement techniques.
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Water Vapor during ICARTT 2004: Comparison of AATS-14, J31 in situ, Ron Brown sonde measurements NASA Ames Airborne Sunphotometer Team SSFR Team Presented by John Livingston SRI International/NASA Ames J31 Data Workshop 9-10Mar05
JETSTREAM-31 during ICARTT 2004 Vaisala HMP243 AATS-14 SSFR
Calculation of columnar water vapor from AATS-14 For the AATS-14 channel centered at 940.6 nm, V Vo exp [-mother] TH2O. LBLRTM V9.2 was used to calculate water vapor transmittance, TH2O, as a function of water vapor slant path, U, by varying the solar zenith angle. Calculations were performed for a variety of model atmospheres and a range of aircraft altitudes. The water vapor transmittance was modeled as TH2O = c exp [-a U b] , where U is the slant path water vapor in [atm-cm].
Calculation of water vapor density from AATS-14 • The columnar water vapor derived from AATS-14 measurements obtained during aircraft vertical profiles is smoothed with a spline fit and then differentiated to yield a corresponding profile of water vapor density. • This profile can be compared with coincident in-situ or remote measurements.
Calculation of relative humidity by the Vaisala HMP243 • HMP243 consists of a heated composite humidity sensor head and an optional sensor head to measure ambient temperature • Both probes mounted on the J31 during the ICARTT study • Primary output is dewpoint, which is calculated within HMP243 from humidity and temperature readings of composite sensor • Separate temp probe permits calculation of ambient relative humidity • HMP243 outputs of ambient temperature, Ttotal, and relative humidity, RHVaisala, were recorded by SSFR data system • Because the separate temperature probe is subject to dynamic heating effects, both Ttotal and RHVaisala must be corrected to account for these effects
Calculation of water vapor density from J31 in-situ measurements • Measured quantities: Pwing, Pnose, TVaisala probe2, RHVaisala
Table of AATS-14 H2O profiles and Ron Brown radiosonde measurements
22.2 km Mean separation: 26.0 km
22 Jul F13 • DC-8 coordination