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The adjoint of the WAM model
This manual gave a description how to use the WamC5 system, which allows for adjoint runs of the ...
H Hersbach | Year: 1997 | Pages: 33
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Detection of lightning-produced NO in the midlatitude upper troposphere during STREAM 1998
Simultaneous in situ measurements of NO, NOy, HNO3, CO, CO2, O3, and aerosols were performed in t...
L Lange, P Hoor, G Helas, H Fischer, D Brunner | Status: published | Journal: J. Geophys. Res. | Volume: 106 | Year: 2001 | First page: 27,777 | Last page: 27,785 | doi: 10.1029/2001JD900210
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An intercomparison of results from three trajectory models
Three three-dimensional trajectory models(LAGRANTO, TRAJKS and FLEXTRA), all driven with analysis...
A Stohl, L Haimberger, MP Scheele, H Wernli | Journal: Meteorol. Appl. | Volume: 8 | Year: 2001 | First page: 127 | Last page: 135
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Preliminary validation results of the OMI O2-O2 cloud product
Cloud correction is an important step in the retrieval process of trace gases from OMI spectra. T...
M Sneep, JP Veefkind, JF de Haan, P Stammes | Conference: Atmospheric Science | Organisation: ESA | Place: ESTEC, Noordwijk, The Netherlands | Year: 2006 | First page: 0 | Last page: 0
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Constraining the Moho depth below Bhutan with global-phase seismic interferometry
We use a novel technique named global-phase seismic interferometry (GloPSI) to image the lithosph...
Anne Obermann, Elmer Ruigrok, Irene Bianchi, György Hetényi | Journal: Front. Earth Sci. | Year: 2021 | doi: https://doi.org/10.3389/feart.2021.658146
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