We compare Tropospheric Emission Spectrometer (TES) versions 3 and 4, V003 and V004, respectively, nadir-stare ozone profiles with ozonesonde profiles from the Arctic Intensive Ozonesonde Network Study (ARCIONS, http://croc.gsfc.nasa.gov/arcions/ during the Arctic Research on the Composition of the Troposphere from Aircraft and Satellites (ARCTAS) field mission. The ozonesonde data are from launches timed to match Aura's overpass, where 11 coincidences spanned 44° N to 71° N from April to July 2008. Using the TES "stare" observation mode, 32 observations are taken over each coincidental ozonesonde launch. By effectively sampling the same air mass 32 times, comparisons are made between the empirically-calculated random errors to the expected...
Ozonesonde observations from Lauder (45.0°S, 169.7°E) and Boulder (39.9°N, 105.3°W) are used to exam...
International audienceVertical profiles of ozone concentration in the high latitudes were observed b...
Initial results are presented on Ozone Monitoring Instrumnet (OMI) validation from the Sodankyla Tot...
We compare Tropospheric Emission Spectrometer (TES) versions 3 and 4, V003 and V004, respectively, n...
Abstract. In this analysis, Tropospheric Emission Spectrometer (TES) V004 nadir ozone (O3) profiles ...
We compare Tropospheric Emission Spectrometer (TES) version 2 (V002) nadir ozone profiles with ozone...
We apply the Tropospheric Emission Spectrometer (TES) ozone retrieval algorithm to Infrared Atmosphe...
(EOS)-Aura spacecraft measures global profiles of atmospheric ozone with vertical resolution of 6–7 ...
We apply the Tropospheric Emission Spectrometer (TES) ozone retrieval algorithm to Infrared Atmosphe...
Of all satellite measurements of ozone, only two instruments have coincident, spatially overlapping ...
We use simultaneous observations of tropospheric ozone and outgoing longwave radiation (OLR) sensiti...
A solar occultation sensor, the Improved Limb Atmospheric Spectrometer (ILAS)-II, measured 5890 vert...
[1] Ozone profiles are derived from back scattered radiance spectra in the ultraviolet (289–339 nm) ...
International audienceThis paper presents a first statistical validation of tropospheric ozone produ...
Ozonesonde observations from Lauder (45.0°S, 169.7°E) and Boulder (39.9°N, 105.3°W) are used to exam...
International audienceVertical profiles of ozone concentration in the high latitudes were observed b...
Initial results are presented on Ozone Monitoring Instrumnet (OMI) validation from the Sodankyla Tot...
We compare Tropospheric Emission Spectrometer (TES) versions 3 and 4, V003 and V004, respectively, n...
Abstract. In this analysis, Tropospheric Emission Spectrometer (TES) V004 nadir ozone (O3) profiles ...
We compare Tropospheric Emission Spectrometer (TES) version 2 (V002) nadir ozone profiles with ozone...
We apply the Tropospheric Emission Spectrometer (TES) ozone retrieval algorithm to Infrared Atmosphe...
(EOS)-Aura spacecraft measures global profiles of atmospheric ozone with vertical resolution of 6–7 ...
We apply the Tropospheric Emission Spectrometer (TES) ozone retrieval algorithm to Infrared Atmosphe...
Of all satellite measurements of ozone, only two instruments have coincident, spatially overlapping ...
We use simultaneous observations of tropospheric ozone and outgoing longwave radiation (OLR) sensiti...
A solar occultation sensor, the Improved Limb Atmospheric Spectrometer (ILAS)-II, measured 5890 vert...
[1] Ozone profiles are derived from back scattered radiance spectra in the ultraviolet (289–339 nm) ...
International audienceThis paper presents a first statistical validation of tropospheric ozone produ...
Ozonesonde observations from Lauder (45.0°S, 169.7°E) and Boulder (39.9°N, 105.3°W) are used to exam...
International audienceVertical profiles of ozone concentration in the high latitudes were observed b...
Initial results are presented on Ozone Monitoring Instrumnet (OMI) validation from the Sodankyla Tot...