JOYCE: Jülich Observatory for Cloud Evolution

U. Löhnert Institute for Geophysics am Meteorology, University of Cologne, Cologne, Germany

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J. H. Schween Institute for Geophysics am Meteorology, University of Cologne, Cologne, Germany

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C. Acquistapace Institute for Geophysics am Meteorology, University of Cologne, Cologne, Germany

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K. Ebell Institute for Geophysics am Meteorology, University of Cologne, Cologne, Germany

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M. Maahn Institute for Geophysics am Meteorology, University of Cologne, Cologne, Germany

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M. Barrera-Verdejo Institute for Geophysics am Meteorology, University of Cologne, Cologne, Germany

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A. Hirsikko Institut für Energie- und Klimaforschung: Troposphäre (IEK-8), Forschungszentrum Jülich GmbH, Jülich, Germany

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B. Bohn Institut für Energie- und Klimaforschung: Troposphäre (IEK-8), Forschungszentrum Jülich GmbH, Jülich, Germany

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A. Knaps Geschäftsbereich Sicherheit und Strahlenschutz (S-UM), Forschungszentrum Jülich GmbH, Jülich, Germany

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E. O’Connor Department of Meteorology, University of Reading, Reading, United Kingdom, and Finnish Meteorological Institute, Helsinki, Finland

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C. Simmer Meteorological Institute, University of Bonn, Bonn, Germany

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A. Wahner Institut für Energie- und Klimaforschung: Troposphäre (IEK-8), Forschungszentrum Jülich GmbH, Jülich, Germany

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S. Crewell Institute for Geophysics am Meteorology, University of Cologne, Cologne, Germany

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Abstract

The Jülich Observatory for Cloud Evolution (JOYCE), located at Forschungszentrum Jülich in the most western part of Germany, is a recently established platform for cloud research. The main objective of JOYCE is to provide observations, which improve our understanding of the cloudy boundary layer in a midlatitude environment. Continuous and temporally highly resolved measurements that are specifically suited to characterize the diurnal cycle of water vapor, stability, and turbulence in the lower troposphere are performed with a special focus on atmosphere–surface interaction. In addition, instruments are set up to measure the micro- and macrophysical properties of clouds in detail and how they interact with different boundary layer processes and the large-scale synoptic situation. For this, JOYCE is equipped with an array of state-of-the-art active and passive remote sensing and in situ instruments, which are briefly described in this scientific overview. As an example, a 24-h time series of the evolution of a typical cumulus cloud-topped boundary layer is analyzed with respect to stability, turbulence, and cloud properties. Additionally, we present longer-term statistics, which can be used to elucidate the diurnal cycle of water vapor, drizzle formation through autoconversion, and warm versus cold rain precipitation formation. Both case studies and long-term observations are important for improving the representation of clouds in climate and numerical weather prediction models.

CORRESPONDING AUTHOR: Dr. Ulrich Löhnert, Institute for Geophysics and Meteorology, Pohligstraße 3, 50969 Köln, Germany, E-mail: loehnert@meteo.uni-koeln.de

Abstract

The Jülich Observatory for Cloud Evolution (JOYCE), located at Forschungszentrum Jülich in the most western part of Germany, is a recently established platform for cloud research. The main objective of JOYCE is to provide observations, which improve our understanding of the cloudy boundary layer in a midlatitude environment. Continuous and temporally highly resolved measurements that are specifically suited to characterize the diurnal cycle of water vapor, stability, and turbulence in the lower troposphere are performed with a special focus on atmosphere–surface interaction. In addition, instruments are set up to measure the micro- and macrophysical properties of clouds in detail and how they interact with different boundary layer processes and the large-scale synoptic situation. For this, JOYCE is equipped with an array of state-of-the-art active and passive remote sensing and in situ instruments, which are briefly described in this scientific overview. As an example, a 24-h time series of the evolution of a typical cumulus cloud-topped boundary layer is analyzed with respect to stability, turbulence, and cloud properties. Additionally, we present longer-term statistics, which can be used to elucidate the diurnal cycle of water vapor, drizzle formation through autoconversion, and warm versus cold rain precipitation formation. Both case studies and long-term observations are important for improving the representation of clouds in climate and numerical weather prediction models.

CORRESPONDING AUTHOR: Dr. Ulrich Löhnert, Institute for Geophysics and Meteorology, Pohligstraße 3, 50969 Köln, Germany, E-mail: loehnert@meteo.uni-koeln.de
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