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EUCLIPSE First Period Report

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instantaneous COSP inputs have to be generated from the model, and then COSP is<br />

run independently.<br />

The latest version of COSP was implemented in the GCMs participating in <strong>EUCLIPSE</strong>,<br />

in fulfilment of Deliverable 1.3. These are the institutes that participated in this task:<br />

• UK Met Office (UKMO),<br />

• Laboratoire de Météorologie Dynamique/Institut Pierre Simon Laplace<br />

(LMD/IPSL),<br />

• Max-Planck Institut für Meteorologie (MPI-M),<br />

• Météo-France Centre National de Recherches Météorologiques (MF-CNRM),<br />

• Koninklijk Nederlands Meteorologisch Instituut (KNMI).<br />

These centres are running the following models as part of <strong>EUCLIPSE</strong>:<br />

• UKMO: HadGEM2<br />

• LMD/IPSL: LMDZ5<br />

• MPI-M: ECHAM6<br />

• MF-CNRM: CNRM-CM5<br />

• KNMI: EC-Earth<br />

COSP was implemented both off- and in-line at UKMO, in line at KNMI, and off-line in<br />

the other three modelling centers. The technical work of the implementation was<br />

aided significantly by the monthly teleconferences established by WP1, which enabled<br />

the group at UKMO (Bojas, Webb) to provide technical assistance to the rest of the<br />

modelling groups. A full report, entitled '<strong>Report</strong> on the implementation of ESM<br />

versions with COSP software, was posted on the <strong>EUCLIPSE</strong> web site<br />

(http://www.euclipse.eu/products.html) in April of 2011, fulfilling the requirement for<br />

Deliverable 1.3. The report shows examples of the COSP outputs for the different<br />

models, with figures showing outputs from the three instrument simulators (ISCCP,<br />

CALIPSO and CloudSat) from which outputs are requested for the <strong>EUCLIPSE</strong><br />

experiments. They show global and tropical (15° S-15° N) averages of the following<br />

variables:<br />

• ISCCP: histograms of cloud top pressure versus optical depth<br />

• CALIPSO: histograms of scattering ratio as a function of height<br />

• CloudSat: histograms of radar reflectivity as a function of height<br />

Here an example is shown of representative COSP output from a run of HadGEM2.<br />

Figure 2 shows COSP outputs from one July of an atmosphere-ocean coupled<br />

simulation of HadGEM2 with preindustrial forcings. The left-hand side column shows<br />

globally-averaged results, and the right-hand side column shows averages over the<br />

tropical belt (15° S-15° N): (a,b) ISCCP histograms, (c,d) CALIPSO histograms, and<br />

(e,f) CloudSat histograms.<br />

In addition to the more complex COSP package, a simpler simulator of MODIS<br />

products was constructed by MPI (Quaas). The simulator allows for a comparison of<br />

climate-model simulated cloud and aerosol fields with retrievals by MODIS and other<br />

space borne passive radiometers. The tool considers three steps: (i) the sampling of<br />

cloud-top quantities using the model's cloud overlap hypothesis, (ii) the satellite<br />

instrument sensitivity by discarding clouds with little cloud fraction or optical depth,<br />

and (iii) the diurnal sampling by taking into account the satellite overpass time for<br />

polar-orbiting satellites. The tool is easy to implement and easy to use, and has been<br />

tested widely.<br />

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