New fast response photofragment fluorescence hygrometer for use on the NASA ER‐2 and the Perseus remotely piloted aircraft
about
Mechanisms controlling water vapor in the lower stratosphere: “A tale of two stratospheres”A new photolysis laser-induced fluorescence instrument for the detection of H2O and HDO in the lower stratosphere.Clarifying the dominant sources and mechanisms of cirrus cloud formation.A new direct absorption tunable diode laser spectrometer for high precision measurement of water vapor in the upper troposphere and lower stratosphere.Evaluation of UT/LS hygrometer accuracy by intercomparison during the NASA MACPEX mission.Definitions and sharpness of the extratropical tropopause: A trace gas perspectiveOn the control of stratospheric humidityA new cavity based absorption instrument for detection of water isotopologues in the upper troposphere and lower stratosphereEffect of convection on the summertime extratropical lower stratosphereMeasurements of stratospheric carbon dioxide and water vapor at northern midlatitudes: Implications for troposphere-to-stratosphere transportMeasurements of water vapor in the tropical lower stratosphere during the CEPEX Campaign: Results and interpretationAn examination of the total hydrogen budget of the lower stratosphereSPADE H2O measurements and the seasonal cycle of stratospheric water vaporHydration, dehydration, and the total hydrogen budget of the 1999/2000 winter Arctic stratosphereComparison between DC-8 and ER-2 species measurements in the tropical middle troposphere: NO, NOy, O3, CO2, CH4, and N2OOH in the tropical upper troposphere and its relationships to solar radiation and reactive nitrogenNitric acid uptake on subtropical cirrus cloud particlesPreface [to special section on Photochemistry of Ozone Loss in the Arctic Region in Summer (POLARIS)]A conceptual model of the dehydration of air due to freeze-drying by optically thin, laminar cirrus rising slowly across the tropical tropopauseClosure of the total hydrogen budget of the northern extratropical lower stratosphereOn the accuracy of in situ water vapor measurements in the troposphere and lower stratosphere with the Harvard Lyman-α hygrometerPhysical processes controlling the spatial distributions of relative humidity in the tropical tropopause layer over the PacificConstraints on the seasonal cycle of stratospheric water vapor using in situ measurements from the ER-2 and a CO photochemical clockThe seasonal cycle of water vapor and saturation vapor mixing ratio in the extratropical lowermost stratosphereEmpirical age spectra for the lower tropical stratosphere from in situ observations of CO2: Implications for stratospheric transportDehydration and denitrification in the Arctic Polar Vortex during the 1995-1996 winterTroposphere-to-stratosphere transport in the lowermost stratosphere from measurements of H2O, CO2, N2O and O3In-situ observations of mid-latitude forest fire plumes deep in the stratosphereEstimates of the seasonal cycle of mass and ozone transport at high northern latitudes
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New fast response photofragment fluorescence hygrometer for use on the NASA ER‐2 and the Perseus remotely piloted aircraft
description
article
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im November 1994 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована в листопаді 1994
@uk
name
New fast response photofragmen ...... seus remotely piloted aircraft
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New fast response photofragmen ...... seus remotely piloted aircraft
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type
label
New fast response photofragmen ...... seus remotely piloted aircraft
@en
New fast response photofragmen ...... seus remotely piloted aircraft
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prefLabel
New fast response photofragmen ...... seus remotely piloted aircraft
@en
New fast response photofragmen ...... seus remotely piloted aircraft
@nl
P2093
P2860
P356
P1476
New fast response photofragmen ...... seus remotely piloted aircraft
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P2093
Andrew E. Dessler
Elliot M. Weinstock
Eric J. Hintsa
James F. Oliver
James G. Anderson
Joseph N. Demusz
Larry B. Lapson
Nathan L. Hazen
Norton T. Allen
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P304
P356
10.1063/1.1144536
P577
1994-11-01T00:00:00Z