17 research outputs found
Special issue “Swarm science results after 2 years in space”
International audienc
The Swarm Initial Field Model for the 2014 geomagnetic field
Data from the first year of ESA's Swarm constellation mission are used to derive the Swarm Initial Field Model (SIFM), a new model of the Earth's magnetic field and its time variation. In addition to the conventional magnetic field observations provided by each of the three Swarm satellites, explicit advantage is taken of the constellation aspect by including east-west magnetic intensity gradient information from the lower satellite pair. Along-track differences in magnetic intensity provide further information concerning the north-south gradient. The SIFM static field shows excellent agreement (up to at least degree 60) with recent field models derived from CHAMP data, providing an initial validation of the quality of the Swarm magnetic measurements. Use of gradient data improves the determination of both the static field and its secular variation, with the mean misfit for east-west intensity differences between the lower satellite pair being only 0.12 nT
ESA's Space-based Doppler Wind Lidar Mission Aeolus - First Wind and Aerosol Product Assessment Results
The European Space Agency (ESA) wind mission,
Aeolus, hosts the first space-based Doppler Wind
Lidar (DWL) world-wide. The primary mission
objective is to demonstrate the DWL technique for
measuring wind profiles from space, intended for
assimilation in Numerical Weather Prediction
(NWP) models. The wind observations will also be
used to advance atmospheric dynamics research
and for evaluation of climate models. Mission spinoff products are profiles of cloud and aerosol
optical properties. Aeolus was launched on 22
August 2018, and the Atmospheric LAser Doppler
INstrument (Aladin) instrument switch-on was
completed with first high energy output in wind
mode on 4 September 2018. The on-ground
data processing facility worked excellent, allowing
L2 product output in near-real-time from the start
of the mission. First results from the wind profile
product (L2B) assessment show that the winds are
of very high quality, with random errors in the free
Troposphere within (cloud/aerosol backscatter
winds: 2.1 m/s) and larger (molecular backscatter
winds: 4.3 m/s) than the requirements (2.5 m/s), but
still allowing significant positive impact in first
preliminary NWP impact experiments. The higher
than expected random errors at the time of writing
are amongst others due to a lower instrument outand input photon budget than designed. The
instrument calibration is working well, and some of
the data processing steps are currently being
refined to allow to fully correct instrument
alignment related drifts and elevated detector dark
currents causing biases in the first data product
version. The optical properties spin-off product
(L2A) is being compared e.g. to NWP model
clouds, air quality model forecasts, and collocated
ground-based observations. Features including
optically thick and thin particle and hydrometeor
layers are clearly identified and are being validated
Initial Assessment of the Performance of the First Wind Lidar in Space on Aeolus
Soon after its successful launch in August 2018,
the spaceborne wind lidar ALADIN (Atmospheric
LAser Doppler INstrument) on-board ESA's
Earth Explorer satellite Aeolus has demonstrated
to provide atmospheric wind profiles on a global
scale. Being the first ever Doppler Wind Lidar
(DWL) instrument in space, ALADIN contributes
to the improvement in numerical weather
prediction (NWP) by measuring one component
of the horizontal wind vector. The performance of
the ALADIN instrument was assessed by a team
from ESA, DLR, industry, and NWP centers
during the first months of operation. The current
knowledge about the main contributors to the
random and systematic errors from the instrument
will be discussed. First validation results from an
airborne campaign with two wind lidars on-board
the DLR Falcon aircraft will be shown