Satellite accelerometers, such as those carried on the CHAMP and GRACE satellites, can provide valuable data for improving our knowledge of thermosphere den-sity and winds. These data are now available over a wide range of the defining conditions, including more than half a solar cycle. Continuity and enhancement of this multi-satellite accelerometer data set will be provided by ESA’s Swarm mission. This paper presents an overview of a 1.5-year ESA-funded study, covering the process-ing steps required for accurately converting accelerome-ter data into density and wind data, and the subsequent use of this data for improving our understanding of the thermosphere. The study concludes with recommenda-tions for the design of future thermosphere ...
The Swarm satellites were launched on November 22, 2013, and carry accelerometers and GPS receivers ...
TND-IGG RL01: This dataset is the first release of thermospheric neutral densities (TND) processed a...
ability to measure the surface forces present. The total density can be easily derived from this mea...
Since 2000, accelerometers on board of the CHAMP, GRACE, GOCE and Swarm satellites have provided hig...
After the detection of many anomalies in the Swarm accelerometer data, an alternative method has bee...
Thermospheric density and wind are important parameters to make accurate life-time estimates for sat...
The thermosphere observations from low-Earth orbiting satellites (TOLEOS) project will provide new t...
The satellite acceleration data from the CHAMP, GRACE, GOCE, and Swarm missions provide detailed inf...
Within the TOLEOS project improved processing standards are used to process GRACE, GRACE-FO and CHAM...
Satellite drag modeling remains the largest source of uncertainty affecting space operations in low ...
Gravity satellite missions measurement data are primarily intended for use in the estimation of an ...
We present new neutral mass density and crosswind observations for the CHAMP, GRACE, and GRACE-FO mi...
We present new neutral mass density and crosswind observations for the CHAMP, GRACE, and GRACE-FO mi...
Accurate forecasts of thermosphere densities, realistic calculation of aerodynamic drag, and propaga...
This thesis is focused on research of an accurate method to compute atmospheric density. It presents...
The Swarm satellites were launched on November 22, 2013, and carry accelerometers and GPS receivers ...
TND-IGG RL01: This dataset is the first release of thermospheric neutral densities (TND) processed a...
ability to measure the surface forces present. The total density can be easily derived from this mea...
Since 2000, accelerometers on board of the CHAMP, GRACE, GOCE and Swarm satellites have provided hig...
After the detection of many anomalies in the Swarm accelerometer data, an alternative method has bee...
Thermospheric density and wind are important parameters to make accurate life-time estimates for sat...
The thermosphere observations from low-Earth orbiting satellites (TOLEOS) project will provide new t...
The satellite acceleration data from the CHAMP, GRACE, GOCE, and Swarm missions provide detailed inf...
Within the TOLEOS project improved processing standards are used to process GRACE, GRACE-FO and CHAM...
Satellite drag modeling remains the largest source of uncertainty affecting space operations in low ...
Gravity satellite missions measurement data are primarily intended for use in the estimation of an ...
We present new neutral mass density and crosswind observations for the CHAMP, GRACE, and GRACE-FO mi...
We present new neutral mass density and crosswind observations for the CHAMP, GRACE, and GRACE-FO mi...
Accurate forecasts of thermosphere densities, realistic calculation of aerodynamic drag, and propaga...
This thesis is focused on research of an accurate method to compute atmospheric density. It presents...
The Swarm satellites were launched on November 22, 2013, and carry accelerometers and GPS receivers ...
TND-IGG RL01: This dataset is the first release of thermospheric neutral densities (TND) processed a...
ability to measure the surface forces present. The total density can be easily derived from this mea...