During November and December 2005, two consortia of mainly European groups conducted an aircraft campaign in Darwin, Australia, to measure the composition of the tropical upper-troposphere and tropopause regions, between 12 and 20 km, in order to investigate the transport and transformation in deep convection of water vapor, aerosols, and trace chemicals. The campaign used two high-altitude aircraft—the Russian M55 Geophysica and the Australian Grob 520 Egrett, which can reach 20 and 15 km, respectively—complemented by upward-pointing lidar measurements from the DLR Falcon and low-level aerosol and chemical measurements from the U.K. Dornier-228. The meteorology during the campaign was characterized mainly by premonsoon conditions—isolated ...
The APE-THESEO campaign was held from 15 February to 15 March 1999 from the Seychelles in the wester...
The case study presented here focuses on the life cycle of clouds in the anvil region of a tropical ...
Abstract. In this study we examine the simulated downward transport and mixing of stratospheric air ...
During November and December 2005, two consortia of mainly European groups conducted an aircraft cam...
An aircraft measurement campaign involving the Russian high-altitude aircraft M55 Geophysica and the...
In the tropics, deep convection is the major source of uncertainty in water vapour transport to the ...
Summaries of flights, instrument usage and Met conditions during the ACTIVE campaigns. ACTIVE ("A...
Summaries of flights, instrument usage and Met conditions during the ACTIVE campaigns. ACTIVE ("A...
Contrails of the Russian high-flying research aircraft M-55 "Geophysica" are investigated in measure...
, is being performed in 2002-2005 in cooperation with the Brazilian pro-ject TROCCIBRAS and in coord...
Abstract. During the SCOUT-O3/ACTIVE field phase in November–December 2005, airborne in situ measure...
In the tropics, deep convection is the major source of uncertainty in water vapor transport to the u...
ACTIVE ("Aerosol and chemical transport in tropical convection") was a NERC-funded consortium projec...
The APE-THESEO campaign was held from 15 February to 15 March 1999 from the Seychelles in the wester...
During the APE-THESEO mission in the Indian Ocean the Myasishchev Design Bureau stratospheric resear...
The APE-THESEO campaign was held from 15 February to 15 March 1999 from the Seychelles in the wester...
The case study presented here focuses on the life cycle of clouds in the anvil region of a tropical ...
Abstract. In this study we examine the simulated downward transport and mixing of stratospheric air ...
During November and December 2005, two consortia of mainly European groups conducted an aircraft cam...
An aircraft measurement campaign involving the Russian high-altitude aircraft M55 Geophysica and the...
In the tropics, deep convection is the major source of uncertainty in water vapour transport to the ...
Summaries of flights, instrument usage and Met conditions during the ACTIVE campaigns. ACTIVE ("A...
Summaries of flights, instrument usage and Met conditions during the ACTIVE campaigns. ACTIVE ("A...
Contrails of the Russian high-flying research aircraft M-55 "Geophysica" are investigated in measure...
, is being performed in 2002-2005 in cooperation with the Brazilian pro-ject TROCCIBRAS and in coord...
Abstract. During the SCOUT-O3/ACTIVE field phase in November–December 2005, airborne in situ measure...
In the tropics, deep convection is the major source of uncertainty in water vapor transport to the u...
ACTIVE ("Aerosol and chemical transport in tropical convection") was a NERC-funded consortium projec...
The APE-THESEO campaign was held from 15 February to 15 March 1999 from the Seychelles in the wester...
During the APE-THESEO mission in the Indian Ocean the Myasishchev Design Bureau stratospheric resear...
The APE-THESEO campaign was held from 15 February to 15 March 1999 from the Seychelles in the wester...
The case study presented here focuses on the life cycle of clouds in the anvil region of a tropical ...
Abstract. In this study we examine the simulated downward transport and mixing of stratospheric air ...