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| 001 | 187197 | ||
| 005 | 20240712100950.0 | ||
| 024 | 7 | _ | |a 10.1175/BAMS-D-14-00105.1 |2 doi |
| 024 | 7 | _ | |a 0003-0007 |2 ISSN |
| 024 | 7 | _ | |a 1520-0477 |2 ISSN |
| 024 | 7 | _ | |a WOS:000359855000001 |2 WOS |
| 024 | 7 | _ | |a 2128/20705 |2 Handle |
| 037 | _ | _ | |a FZJ-2015-00871 |
| 082 | _ | _ | |a 550 |
| 100 | 1 | _ | |a Löhnert, U. |0 P:(DE-Juel1)129225 |b 0 |e Corresponding Author |u fzj |
| 245 | _ | _ | |a JOYCE: Juelich Observatory for Cloud Evolution |
| 260 | _ | _ | |a Boston, Mass. |c 2014 |b ASM |
| 336 | 7 | _ | |a article |2 DRIVER |
| 336 | 7 | _ | |a Output Types/Journal article |2 DataCite |
| 336 | 7 | _ | |a Journal Article |b journal |m journal |0 PUB:(DE-HGF)16 |s 1441182566_13301 |2 PUB:(DE-HGF) |
| 336 | 7 | _ | |a ARTICLE |2 BibTeX |
| 336 | 7 | _ | |a JOURNAL_ARTICLE |2 ORCID |
| 336 | 7 | _ | |a Journal Article |0 0 |2 EndNote |
| 520 | _ | _ | |a 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. |
| 536 | _ | _ | |a 233 - Trace gas and aerosol processes in the troposphere (POF2-233) |0 G:(DE-HGF)POF2-233 |c POF2-233 |f POF II |x 0 |
| 588 | _ | _ | |a Dataset connected to CrossRef, juser.fz-juelich.de |
| 700 | 1 | _ | |a Schween, J. H. |0 P:(DE-HGF)0 |b 1 |
| 700 | 1 | _ | |a Acquistapace, C. |0 P:(DE-HGF)0 |b 2 |
| 700 | 1 | _ | |a Ebell, K. |0 P:(DE-HGF)0 |b 3 |
| 700 | 1 | _ | |a Maahn, M. |0 P:(DE-HGF)0 |b 4 |
| 700 | 1 | _ | |a Barreraverdejo, M. |0 P:(DE-HGF)0 |b 5 |
| 700 | 1 | _ | |a Hirsikko, A. |0 P:(DE-Juel1)157625 |b 6 |u fzj |
| 700 | 1 | _ | |a Bohn, B. |0 P:(DE-Juel1)2693 |b 7 |u fzj |
| 700 | 1 | _ | |a Knaps, A. |0 P:(DE-Juel1)133467 |b 8 |u fzj |
| 700 | 1 | _ | |a O'connor, E. |0 P:(DE-HGF)0 |b 9 |
| 700 | 1 | _ | |a Simmer, C. |0 P:(DE-HGF)0 |b 10 |
| 700 | 1 | _ | |a Wahner, A. |0 P:(DE-Juel1)16324 |b 11 |u fzj |
| 700 | 1 | _ | |a Crewell, S. |0 P:(DE-HGF)0 |b 12 |
| 773 | _ | _ | |a 10.1175/BAMS-D-14-00105.1 |g p. 141104074432007 - |0 PERI:(DE-600)2029396-3 |n 7 |p 1157–1174 |t Bulletin of the American Meteorological Society |v 96 |y 2014 |x 1520-0477 |
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