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KONTROL 1984 - First Experiment on Convection and Turbulence over the North Sea: radiosoundings at the research vessel Valdivia

KONTROL 1984 is part of research activities focused on organized convection phenomena as they are often manifested in organized cloud patterns like the well-known boundary layer cloud streets or open and closed cellular cloud structures.


The experimental part of the investigations began with the experiment KonTur (Konvektion and Turbulenz) in September and October 1981. It continued with the experiments KONTROL in August 1984 and KONTROL in October 1985. All experiments took place over the German Bight in the southeastern part of the North Sea.


The experimental concept based on the use of two fixed stations performing continuous aerological and surface observations and two aircraft conducting detailed observations during special periods. The stations were the research vessel Valdivia and the research platform NORDSEE (54°42'N, 7°10'E). The aircraft were a FALCON-20 of DFVLR and a DO-28 Skyservant of the TU Braunschweig.

Simple

Date (Publication)
2012-03-28
Edition

1

Citation identifier
UNI_HH_MI_KONTROL1984
Citation identifier
doi:10.1594/WDCC/UNI_HH_MI_KONTROL1984
Originator
  University of Hamburg - Dr. Gerd Müller
http://www.mi.uni-hamburg.de/
Author
  University of Hamburg - Heinrich Hoeber
http://www.mi.uni-hamburg.de/
Author
  Max Planck Institute for Meteorology - Gottfried Kruspe
http://www.mpimet.mpg.de/
Author
  University of Hamburg - Prof. Dr. Burghard Brümmer
http://www.mi.uni-hamburg.de/
Author
  University of Hamburg - Christian Wetzel
http://www.mi.uni-hamburg.de/
Principal investigator
  University of Hamburg - Prof. Dr. Burghard Brümmer
http://www.mi.uni-hamburg.de/
Publisher
  WDC Climate at DKRZ
Point of contact
  University of Hamburg - Dr. Gerd Müller
http://www.mi.uni-hamburg.de/
Name

tar-File(s)

Keywords
  • observational data

Keywords
  • radiosonde

Keywords
  • ship

Use limitation

scientific use: For scientific use only

Language

eng; USA

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Begin date
1984-08-06
End date
1984-08-24
Distribution format
  • tar-File(s) ()

Transfer size
2
OnLine resource
https://www.wdc-climate.de/ui/entry?acronym=UNI_HH_MI_KONTROL1984
Hierarchy level
collection

Completeness commission

Name of measure

n/a

Measure description

None

Non quantitative attribute accuracy

Name of measure

n/a

Measure description

None

Attribute description
height
Descriptor

Height is the vertical distance above the surface. [CF-Standard Name]; unit: m

Attribute description
relative_humidity
Descriptor

relative_humidity [CF-Standard Name]; unit: not filled

Attribute description
specific_humidity
Descriptor

"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: g kg-1

Attribute description
air_pressure
Descriptor

air_pressure [CF-Standard Name]; unit: hPa

Attribute description
dew_point_temperature
Descriptor

Dew point temperature is the temperature at which a parcel of air reaches saturation upon being cooled at constant pressure and specific humidity. [CF-Standard Name]; unit: not filled

Attribute description
wind_speed
Descriptor

Speed is the magnitude of velocity. Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) The wind speed is the magnitude of the wind velocity.[CF-Standard Name]; unit: m s-1

Attribute description
air_temperature
Descriptor

Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: not filled

Attribute description
wind_from_direction
Descriptor

Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) In meteorological reports, the direction of the wind vector is usually (but not always) given as the direction from which it is blowing (wind_from_direction) (westerly, northerly, etc.). In other contexts, such as atmospheric modelling, it is often natural to give the direction in the usual manner of vectors as the heading or the direction to which it is blowing (wind_to_direction) (eastward, southward, etc.) "from_direction" is used in the construction X_from_direction and indicates the direction from which the velocity vector of X is coming. [CF-Standard Name]; unit: degree

File identifier
wdc-climate.de:2250990 XML
Metadata language

eng; USA

Hierarchy level
collection
Hierarchy level name

UNI_HH_MI_KONTROL1984

Date stamp
2011-06-22T14:52:12
Metadata standard name

ISO 19115

Metadata standard version

ISO 19115-2:2009

Point of contact
  University of Hamburg - Christian Wetzel
http://www.mi.uni-hamburg.de/
Point of contact
  University of Hamburg - Dr. Gerd Müller
http://www.mi.uni-hamburg.de/
 
 

Overviews

Spatial extent

N
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E
W
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Keywords


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