Clear-sky closure studies of lower tropospheric aerosol and water vapor during ACE-2 using airborne sunphotometer, airborne in-situ, space-borne, andground-based measurements
B. Schmid et al., Clear-sky closure studies of lower tropospheric aerosol and water vapor during ACE-2 using airborne sunphotometer, airborne in-situ, space-borne, andground-based measurements, TELLUS B, 52(2), 2000, pp. 568-593
We report on clear-sky column closure experiments (CLEARCOLUMN) performed i
n the Canary Islands during the second Aerosol Characterization Experiment
(ACE-2) in June/July 1997. We present CLEARCOLUMN results obtained by combi
ning airborne sunphotometer and in-situ (optical particle counter, nephelom
eter, and absorption photometer) measurements taken aboard the Pelican airc
raft, space-borne NOAA/AVHRR data and ground-based lidar and sunphotometer
measurements. During both days discussed here, vertical profiles flown in c
loud-free air masses revealed 3 distinctly different layers: a marine bound
ary layer (MBL) with varying pollution levels, an elevated dust layer, and
a very clean layer between the MBL and the dust layer. A key result of this
study is the achievement of closure between extinction or layer aerosol op
tical depth (AOD) computed from continuous in-situ aerosol size-distributio
ns and composition and those measured with the airborne sunphotometer. In t
he dust, the agreement in layer AOD (lambda = 380 1060 nm) is 3-8%. In the
MBL there is a tendency for the in-situ results to be slightly lower than t
he sunphotometer measurements (10 17% at lambda = 525 nm), but those differ
ences are within the combined error bars of the measurements and computatio
ns.