Add to ORKGThe ESRAD 52 MHz MST radar (67° 53 ‘ N, 21 ° 06 ‘ E) has observed thin layers of enhanced radar echo...
The Earth's mesosphere is the region of the atmosphere between approximately 60-120 km altitude, whe...
On 30 October 2004 during a strong solar proton event, layers of enhanced backscatter from altitude...
Large amounts of meteoric particles ablate globally into the Earth’s atmosphere each day, and they i...
18th EISCAT symposiumSession E3: Ionoshere/thermosphere/mesosphereMay 27 (Sat), NIPR Auditoriu
18th EISCAT symposiumSession E3: Ionoshere/thermosphere/mesosphereMay 27 (Sat), Poster Sessio
We discuss the influence of charged dust on radar observations in the Earth ionosphere. This region ...
The overall goal of the Aeronomy of Ice in the Mesosphere (AIM) experiment is to resolve why Polar M...
This PhD thesis deals with phenomena which are closely related to the unique thermal structure of th...
The ESRAD 52 MHz MST radar (67 ° 53 ‘ N, 21 ° 06 ‘ E) has observed thin layers of enhanced radar ech...
Polar mesosphere summer echoes (PMSE) are very strong radar echoes primarily studied in the VHF wave...
This Master thesis examines a phenomenon that occurs in the upper polar atmosphere, namely, Polar Me...
Polar Mesospheric Winter Echoes (PMWE) are strong coherent radar echoes, from the upper mesosphere a...
We review some of the work performed over the past two decades with rocket-borne detectors to study ...
Two sounding rocket payloads were launched from Andøya Space Centre (69.29 N, 16.02 E) during the su...
The ESRAD 52 MHz MST radar (67° 53 ‘ N, 21 ° 06 ‘ E) has observed thin layers of enhanced radar echo...
The Earth's mesosphere is the region of the atmosphere between approximately 60-120 km altitude, whe...
On 30 October 2004 during a strong solar proton event, layers of enhanced backscatter from altitude...
Large amounts of meteoric particles ablate globally into the Earth’s atmosphere each day, and they i...
18th EISCAT symposiumSession E3: Ionoshere/thermosphere/mesosphereMay 27 (Sat), NIPR Auditoriu
18th EISCAT symposiumSession E3: Ionoshere/thermosphere/mesosphereMay 27 (Sat), Poster Sessio
We discuss the influence of charged dust on radar observations in the Earth ionosphere. This region ...
The overall goal of the Aeronomy of Ice in the Mesosphere (AIM) experiment is to resolve why Polar M...
This PhD thesis deals with phenomena which are closely related to the unique thermal structure of th...
The ESRAD 52 MHz MST radar (67 ° 53 ‘ N, 21 ° 06 ‘ E) has observed thin layers of enhanced radar ech...
Polar mesosphere summer echoes (PMSE) are very strong radar echoes primarily studied in the VHF wave...
This Master thesis examines a phenomenon that occurs in the upper polar atmosphere, namely, Polar Me...
Polar Mesospheric Winter Echoes (PMWE) are strong coherent radar echoes, from the upper mesosphere a...
We review some of the work performed over the past two decades with rocket-borne detectors to study ...
Two sounding rocket payloads were launched from Andøya Space Centre (69.29 N, 16.02 E) during the su...
The ESRAD 52 MHz MST radar (67° 53 ‘ N, 21 ° 06 ‘ E) has observed thin layers of enhanced radar echo...
The Earth's mesosphere is the region of the atmosphere between approximately 60-120 km altitude, whe...
On 30 October 2004 during a strong solar proton event, layers of enhanced backscatter from altitude...