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Recent results from the Ozone Monitoring Instrument (OMI) on EOS Aura
The Ozone Monitoring Instrument (OMI) is first-of-its-kind hyperspectral instrument that employs ...
PK Bhartia, PF Levelt, J Tamminen, O Torres | Journal: Proc. SPIE Asia-Pacific Remote Sensing Symp. 2006 | Volume: 6408 | Year: 2006 | doi: 10.1117/12.706521
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Overview of the O3M SAF GOME-2 operational atmospheric composition and UV radiation data products and data availability
The three Global Ozone Monitoring Experiment-2 instruments will provide unique and long data sets...
S Hassinen, P Stammes, LG Tilstra | Status: published | Journal: Atmospheric Measurement Techniques | Volume: 9 | Year: 2016 | First page: 383 | Last page: 407 | doi: 10.5194/amt-9-383-2016
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The effect of differences between rainfall measurement techniques on groundwater and discharge simulations in a lowland catchment
Several rainfall measurement techniques are available for hydrological applications, each with it...
CC Brauer, A Overeem, H Leijnse, R Uijlenhoet | Status: published | Journal: Hydrol. Proc. | Volume: 30 | Year: 2016 | First page: 3885 | Last page: 3900 | doi: 10.1002/hyp.10898
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Evaluation of near-surface ozone over Europe from the MACC reanalysis
This work is an extended evaluation of near-surface ozone as part of the global reanalysis of atm...
E Katragkou, P Zanis, A Tsikerdekis, J Kapsomenakis, D Melas, H Eskes, J Flemming, V Huijnen, A Inness, M Schultz, O Stein, C Zerefos | Status: published | Journal: Geoscientific Model Development | Year: 2015 | First page: 2299 | Last page: 2314 | doi: www.geosci-model-dev.net/8/2299/2015/
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Imaging Torfajökull's magmatic plumbing system with seismic interferometry and phase velocity surface wave tomography
Torfajökull volcano, Iceland, has not erupted since 1477. However, intense geothermal activity, d...
JE Martins, EN Ruigrok, D Draganov, A Hooper, RF Hanssen, RS White, H Soosalu | Status: published | Journal: J. Geophys. Res. | Volume: 124 | Year: 2019 | First page: 2920 | Last page: 2940 | doi: 10.1029/2018JB016002
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