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04_OCT2013_ESA-EO_programmes.pdf
ESA EO missions and their exploitation for science and applications ESA
A Guide to Aeolus Range Bin Settings
Current Range Bin Settings Multiple Aeolus Range Bin Settings are active at the same time.
Aeolus
This is currently the only technology that can provide direct wind profile observations in clear air, inside thin clouds
Aeolus 4th Reprocessing Verification Report
This document is a report on Aeolus Data Innovation Science Cluster DISC
Aeolus activates new range bin setting
stratosphere coupled with an overlying westerly jet moving gradually upwards, countering the expected downward propagation of the current
Aeolus ALADIN Monthly L2B Report 01 Aug 2021
These bias jumps have been traced to be associated with fluctuations in the dark current levels on existing hot pixels.
Aeolus ALADIN Monthly L2B Report 01 Jun 2021
It may be due to a wind-speed dependent bias issue that the L2B team are currently working on and hoping to resolve soon
Aeolus ALADIN Monthly L2B Report 01 Jun 2022
amount of solar background noise over the Northern Hemisphere summer solstice, which is a very dominant error term with our current
Aeolus ALADIN Monthly L2B Report 01 May 2021
It may be due to a wind-speed dependent bias issue that the L2B team are currently working on and hoping to resolve soon
Aeolus ALADIN Monthly L2B Report 01 May 2022
maximum amount of solar background noise over the Northern Hemisphere summer, which is a very dominant error term with our current
Aeolus ALADIN Monthly L2B Report 01 Oct 2020
This is being investigated, but it is currently thought to be a seasonal effect (worse in Autumn).
Aeolus ALADIN Monthly L2B Report 01 Sep 2021
These bias jumps have been traced to fluctuations in the dark current levels on existing hot pixels.
Aeolus Data
Aeolus Quality Control Reports on L1B/Instrument, L2A and L2B products are currently available to Aeolus Cal/Val teams and
Aeolus data now publicly available
Following the introduction in June 2019 of a correction of biases related to spectrometer pixels showing elevated dark current
Aeolus enhances volcanic ash forecasts for aviation safety
Currently, wind profile measurements are obtained from radiosondes, commercial aircraft ascents and descents and ground-based
Aeolus Level 2A Algorithm Theoretical Baseline Document – AEL-FM and AEL-PRO products
This document describes Aeolus L2A Algorithm Theoretical Baseline
Aeolus Level 2A Algorithm Theoretical Baseline Document – SCA and MLE products
This document describes Aeolus L2A Algorithm Theoretical Baseline
Aeolus Online Dissemination Help Page
Important Note: the Catalogue Search function is currently not enabled for L1B and L2B Wind data collections which are publicly
Aeolus Overview
Currently, the global distribution of conventional wind profile measurements is not homogenous and mainly located over land
Aeolus_ATBD_Level_1B_Products.pdf
Aeolus L1B Algorithm Theoretical Baseline Document - Level 1B Processor Algorithm Description