The German Aerospace Center (DLR)

Member of the UFS-Consortium

The German Aerospace Center (DLR)

The German Aerospace Center (DLR) is Germany´s national research center for aeronautics and space. Its extensive research and development activities in aeronautics, space, energy, transport and security are integrated into national and international cooperative ventures. As Germany´s space agency, DLR has been given responsibility for the planning and the implementation of the German space programe by the German federal government.

The German Remote Sensing Data Center (DLR-DFD)

Global monitoring of the upper atmosphere - Network for the Detection of Mesopause Change (NDMC)

NDMC is a global program with the mission to promote international cooperation amongst research groups investigating the mesopause region (80-100 km), with the goal of early identification of changing climate signals. This program involves the coordinated study of atmospheric variability at all time scales, the exchange of existing know-how, and the coordinated development of improved observation, analysis techniques and modeling. The initial emphasis is on mesopause region airglow techniques utilizing the existing ground-based and satellite measurement capabilities. NDMC is coordinated by DLR-DFD in cooperation with the UFS.

The German Remote Sensing Data Center (DLR-DFD)

Airglow observations with BAIER (Bavarian Airglow Imager)

The airglow imager instrument BAIER observes the so-called airglow (or nightglow) emission in the middle atmosphere since 2013 almost every night. Airglow is a collective term for emissions due to chemical processes in the middle atmosphere which form (mostly) narrow layers. Many of these emissions are very faint in the visible and can be observed best in the near infrared spectral range. BAIER specifically observes the airglow emissions due to the O2 molecules at 865 nm which comes from an altitude of about 94 km and due to the OH molecule between 715nm and 930 nm which comes from about 87km altitude. The observations of the airglow emissions allow to investigate atmospheric dynamics in the middle atmosphere which is mainly characterized by gravity waves, because the chemical reactions taking place are influenced e.g. by the temperature and pressure changes induced by the gravity waves passing through these emission layers. Gravity waves influence the atmosphere in various ways. On small scales they can lead to local occurrences of turbulence while on global scale they influence weather and climate by distributing energy and momentum in the atmosphere and drive global circulations like the jet streams. Knowledge about the gravity waves especially in the height region of the airglow layers which are used to be able to investigate the gravity waves is important for more precise climate and weather models.

Measurements of the mesopause temperature using the IR-spectrometer GRIPS

The GRIPS (Ground-based Infrared P-branch Spectrometer) instrument routinely measures the temperature in ~87 km altitude with high temporal resolution and precision. The temperatures are used for an early identification of changing climate signals and for the detection of atmospheric gravity waves and infrasound. The latter ones are generated by storm systems, volcanic activity and even tsunamis, and may be used for the rapid detection of natural hazards. Therefore, a deeper understanding of the propagation of these signals through the atmosphere is needed . This is modelled using the HARPA/DLR model.

The Remote Sensing Technology Institute (DLR-IMF)

Max-DOAS measurements of atmospheric trace gases

Multi-axis differential optical absorption spectroscopy (MAX-DOAS) is used to measure stratospheric and tropospheric trace gases including Ozone, NO2, SO2, Formaldehyde, HONO and aerosols. The MAX-DOAS instrument is operated in cooperation with the DWD at the UFS. The DLR-IMF is responsible for the retrieval of trace gas concentrations from slant column densities measured in scattered solar light.

The Institute of Atmospheric Physics (DLR-IPA)

Cloud Microphysics

Precipitation is dependent on the microphysical properties of the clouds. The doppler cloud radar installed at the UFS Schneefernerhaus detects the backscatter signal produced by different hydrometeor types like cloud droplets, drizzle, rain drops, ice particles and snow. This data can help to understand the generation of precipitation and may also be used to validate satellite measurements.

MIRA-36 Cloud Radar at Schneefernerhaus

DLR Micro Rain Radar MRR-2 and Parsivel Disdrometer at Schneefernerhaus