On 30 June 2016 a layer of dust, possibly meteoric smoke particles (MSPs), was observed with a rocket borne probe at 69.29°N, 16.02°E and altitudes of ~74 km where patchy thin cloud layers, detected with the Middle Atmosphere Alomar Radar System, were present. The rocket traversed a layer with a net positive dust charge density of ~10⁷ unit charges per cubic meters and a number density of neutral dust particles with sizes ≥4 nm of ~10⁸ m−³. The positive charge density may require that elements that lower the photoelectric work function coat MSPs. The presence of this relatively large dust is consistent with smaller MSPs being swept out of the low mesospheric cloud region during the summer, while larger MSPs remain where their fall velocitie...
We review some of the work performed over the past two decades with rocket-borne detectors to study ...
We present a new method of analyzing measurements of mesospheric dust made with DUSTY rocket-borne F...
We propose that dust formed at the cool summer mesopause may have optical properties very different ...
On 30 June 2016 a layer of dust, possibly meteoric smoke particles (MSPs), was observed with a rocke...
On 30 June 2016 a layer of dust, possibly meteoric smoke particles (MSPs), was observed with a rocke...
Two sounding rocket payloads were launched from Andøya Space Centre (69.29 N, 16.02 E) during the su...
Ice particles populating noctilucent clouds and being responsible for polar mesosphericsummer echoes...
The Smoke Particle Impact Detector (SPID), newly designed at the University of Tromsø, was launched ...
The Earth's mesosphere is the region of the atmosphere between approximately 60-120 km altitude, whe...
Abstract. The dust detector on the ESPRIT rocket detected two extended dust/aerosol layers during th...
We present results of in situ measurements of mesosphere-lower thermosphere dusty-plasma densities i...
Large amounts of meteoric particles ablate globally into the Earth’s atmosphere each day, and they i...
We present in situ measurements of small-scale fluctuations in aerosol populations as recorded throu...
We present in situ measurements of small-scale fluctuations in aerosol populations as recorded throu...
Submicron aerosols, as evidenced by the occurrence of polar mesospheric and noctilucent clouds, exis...
We review some of the work performed over the past two decades with rocket-borne detectors to study ...
We present a new method of analyzing measurements of mesospheric dust made with DUSTY rocket-borne F...
We propose that dust formed at the cool summer mesopause may have optical properties very different ...
On 30 June 2016 a layer of dust, possibly meteoric smoke particles (MSPs), was observed with a rocke...
On 30 June 2016 a layer of dust, possibly meteoric smoke particles (MSPs), was observed with a rocke...
Two sounding rocket payloads were launched from Andøya Space Centre (69.29 N, 16.02 E) during the su...
Ice particles populating noctilucent clouds and being responsible for polar mesosphericsummer echoes...
The Smoke Particle Impact Detector (SPID), newly designed at the University of Tromsø, was launched ...
The Earth's mesosphere is the region of the atmosphere between approximately 60-120 km altitude, whe...
Abstract. The dust detector on the ESPRIT rocket detected two extended dust/aerosol layers during th...
We present results of in situ measurements of mesosphere-lower thermosphere dusty-plasma densities i...
Large amounts of meteoric particles ablate globally into the Earth’s atmosphere each day, and they i...
We present in situ measurements of small-scale fluctuations in aerosol populations as recorded throu...
We present in situ measurements of small-scale fluctuations in aerosol populations as recorded throu...
Submicron aerosols, as evidenced by the occurrence of polar mesospheric and noctilucent clouds, exis...
We review some of the work performed over the past two decades with rocket-borne detectors to study ...
We present a new method of analyzing measurements of mesospheric dust made with DUSTY rocket-borne F...
We propose that dust formed at the cool summer mesopause may have optical properties very different ...