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        <title>InScAPE</title>
        <description></description>
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        <title>InScAPE</title>
        <link>https://atmos.meteo.uni-koeln.de/inscape/</link>
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        <dc:date>2024-01-26T18:20:46+00:00</dc:date>
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        <title>arcticclouds</title>
        <link>https://atmos.meteo.uni-koeln.de/inscape/doku.php?id=arcticclouds&amp;rev=1706293246&amp;do=diff</link>
        <description>Arctic clouds

[Low-level clouds observed on Svalbard]

Arctic climate features an abundance of low-level clouds. It is well known from scientific studies in the past that these clouds can significantly affect the radiative energy budget of the atmosphere and at the surface. For these reasons it can be expected that low-level clouds could play an important role in the currently ongoing warming of the Arctic climate, a process also known as Arctic Amplification.</description>
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    <item rdf:about="https://atmos.meteo.uni-koeln.de/inscape/doku.php?id=blender&amp;rev=1663165005&amp;do=diff">
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        <dc:date>2022-09-14T14:16:45+00:00</dc:date>
        <dc:creator>Anonymous (anonymous@undisclosed.example.com)</dc:creator>
        <title>blender</title>
        <link>https://atmos.meteo.uni-koeln.de/inscape/doku.php?id=blender&amp;rev=1663165005&amp;do=diff</link>
        <description>Blender

Where graphic design meets atmospheric science

We make use of Blender and its path-tracing engine to realistically render three-dimensional cloud fields from Large-Eddy Simulations (LES). These are not just for show, but can also be used as</description>
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        <dc:date>2021-09-24T09:25:09+00:00</dc:date>
        <dc:creator>Anonymous (anonymous@undisclosed.example.com)</dc:creator>
        <title>cloudfeedbacks</title>
        <link>https://atmos.meteo.uni-koeln.de/inscape/doku.php?id=cloudfeedbacks&amp;rev=1632475509&amp;do=diff</link>
        <description>Cloud feedbacks

Cloud climate feedbacks



Figure 3. The change in cloud fraction (left) and cloud liquid condensate (right) between the future climate (AMIP4K) and present-day climate (AMIP) at the Barbados Cloud Observatory (BCO), for the dry season. The EC-EARTH GCM simulations for the CFMIP5 project are shown in blue, while its SCM forced with cfSites data is shown in red. The solid line is the 30-year average value and the shadowed region displays the variability between monthly samples, c…</description>
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        <dc:date>2022-09-14T14:24:44+00:00</dc:date>
        <dc:creator>Anonymous (anonymous@undisclosed.example.com)</dc:creator>
        <title>cloudscheme</title>
        <link>https://atmos.meteo.uni-koeln.de/inscape/doku.php?id=cloudscheme&amp;rev=1663165484&amp;do=diff</link>
        <description>PDF cloud scheme

Our research into cloud schemes focuses on how to represent clouds and cloud processes in numerical models which do not have sufficient resolution to resolve clouds. As both weather forecast or climate models fall into this category this research has high societal and academic relevance.</description>
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        <dc:date>2022-09-14T15:47:32+00:00</dc:date>
        <dc:creator>Anonymous (anonymous@undisclosed.example.com)</dc:creator>
        <title>edmf</title>
        <link>https://atmos.meteo.uni-koeln.de/inscape/doku.php?id=edmf&amp;rev=1663170452&amp;do=diff</link>
        <description>EDMF

The basics



 Figure 1. Visualization of the EDMF approach in parameterizing the vertical transport by turbulence and convection in the atmosphere.

Large-scale circulation models used for Numerical Weather Prediction (NWP) and climate simulation are formulated in terms of budget equations for a set of conserved state variables $\phi$\begin{eqnarray*}
\frac{D \phi}{D t} = S_{\phi}
\end{eqnarray*}$S_{\phi}$$\phi$\begin{eqnarray*}
S_{\phi,tc} = - \frac{\partial \overline{w&#039;\phi&#039;}}{\partial …</description>
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        <dc:format>text/html</dc:format>
        <dc:date>2021-09-24T12:23:26+00:00</dc:date>
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        <title>greyzone</title>
        <link>https://atmos.meteo.uni-koeln.de/inscape/doku.php?id=greyzone&amp;rev=1632486206&amp;do=diff</link>
        <description>Convective Grey Zone



Figure 1. Visualization of the grey zone in turbulent transport in a subtropical marine shallow cumulus topped boundary layer. Shown is the ratio of the subgrid flux to the total flux as a function of horizontal resolution of a series of LES simulations of the RICO shallow cumulus case, featuring a scale-adaptive version of the EDMF scheme. The intermediate values reflect the range of resolutions at which the resolved contribution is as large as the subgrid contribution, …</description>
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        <dc:format>text/html</dc:format>
        <dc:date>2024-01-23T13:29:24+00:00</dc:date>
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        <title>information</title>
        <link>https://atmos.meteo.uni-koeln.de/inscape/doku.php?id=information&amp;rev=1706016564&amp;do=diff</link>
        <description>Who we are

We are a research group within the Institute of Geophysics and Meteorology of the University of Cologne.



You can find more information about the institute on the  official website. More information about the people in our group can be found staff overview.

[ group photo]

Address</description>
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        <dc:date>2023-07-12T16:00:31+00:00</dc:date>
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        <title>models</title>
        <link>https://atmos.meteo.uni-koeln.de/inscape/doku.php?id=models&amp;rev=1689177631&amp;do=diff</link>
        <description>Models

Our group use a wide range of numerical models of atmosphere, from regional models to large eddy simulations and single column models. 

DALES

The Dutch Atmospheric Large-Eddy Simulation (DALES) model is one of the two large eddy simulations (LES) codes employed at InScAPE. A library of prototype cases is used for research and for further code development, including convective cases as well as cases of stratiform clouds. Many of these have been developed within the context of internatio…</description>
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        <dc:date>2022-09-14T15:55:53+00:00</dc:date>
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        <title>narvalsimulations</title>
        <link>https://atmos.meteo.uni-koeln.de/inscape/doku.php?id=narvalsimulations&amp;rev=1663170953&amp;do=diff</link>
        <description>Simulations for meteorological field campaigns

NARVAL I and II

The first Next-generation Aircraft Remote sensing for VAlidation Studies (NARVAL I) Campaign took place in December 2013 and January 2014. It was divided into NARVAL South, in Barbados, and NARVAL North, in Iceland, respectively. $^3$</description>
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        <dc:date>2022-09-14T15:36:05+00:00</dc:date>
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        <title>population</title>
        <link>https://atmos.meteo.uni-koeln.de/inscape/doku.php?id=population&amp;rev=1663169765&amp;do=diff</link>
        <description>Cloud Population Dynamics

BiOMi (Binomials on Microgrids)

Neggers and Griewank (2021)

The spatial patterns in cumulus cloud populations are a key factor in understanding cloud-climate feedback and cloud-circulation coupling. BiOMi (Binomial Objects on Microgrids) is a toy model developed to recreate populations of interacting convective objects distributed over a two-dimensional Eulerian grid.</description>
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        <dc:format>text/html</dc:format>
        <dc:date>2021-09-24T12:47:27+00:00</dc:date>
        <dc:creator>Anonymous (anonymous@undisclosed.example.com)</dc:creator>
        <title>projects</title>
        <link>https://atmos.meteo.uni-koeln.de/inscape/doku.php?id=projects&amp;rev=1632487647&amp;do=diff</link>
        <description>Research projects

The InScAPE research group has been or is currently involved in the following research projects:

	*  (AC)3 ; &lt;http://www.ac3-tr.de/&gt; 
	*  ASR : &lt;https://asr.science.energy.gov/news/program-news/post/9198&gt;
	*  DFG : ORCA2: &lt;https://gepris.dfg.de/gepris/projekt/442649391&gt;
	*  DFG : POPC4OM, &lt;https://gepris.dfg.de/gepris/projekt/434804401&gt;
	*  DFG : SOCLES, &lt;https://gepris.dfg.de/gepris/projekt/430226822&gt;
	*  DFG : SPP HALO: &lt;http://www.halo-spp.de/&gt;
	*  ET-CC : &lt;http://et-cc.un…</description>
    </item>
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        <dc:format>text/html</dc:format>
        <dc:date>2026-04-01T07:43:32+00:00</dc:date>
        <dc:creator>Anonymous (anonymous@undisclosed.example.com)</dc:creator>
        <title>publications</title>
        <link>https://atmos.meteo.uni-koeln.de/inscape/doku.php?id=publications&amp;rev=1775029412&amp;do=diff</link>
        <description>Publications

2026

Paulus, F. M., Müller, J. J., Kirbus, B., Sodemann, H., van Gelder, L., Walbröl, A., Wendisch, M., and Neggers, R. A. J.: Impacts of mesoscale atmospheric subsidence on cloud glaciation and decoupling in Arctic marine cold air outbreaks.</description>
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        <dc:format>text/html</dc:format>
        <dc:date>2021-04-27T16:38:16+00:00</dc:date>
        <dc:creator>Anonymous (anonymous@undisclosed.example.com)</dc:creator>
        <title>sidebar</title>
        <link>https://atmos.meteo.uni-koeln.de/inscape/doku.php?id=sidebar&amp;rev=1619541496&amp;do=diff</link>
        <description>General

	*  Introduction

	*  Who we are

	*  Research projects

	*  Publications

	*  Student projects

	*  Open positions

Research

	*  Arctic Clouds

	*  Blender

	*  Cloud Geometry

	*  Cloud Feedbacks

	*  Cloud Schemes

	*  EDMF

	*  Field Campaigns 

	*  Grey Zone

	*  Population Dynamics

Tools

	*  Models

	*  Testbed

Code

	*  Binomial sampling

Internal</description>
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        <dc:format>text/html</dc:format>
        <dc:date>2022-09-14T14:42:35+00:00</dc:date>
        <dc:creator>Anonymous (anonymous@undisclosed.example.com)</dc:creator>
        <title>sizedistribution</title>
        <link>https://atmos.meteo.uni-koeln.de/inscape/doku.php?id=sizedistribution&amp;rev=1663166555&amp;do=diff</link>
        <description>Cloud geometry

The earth´s radiation budget is heavily influenced by the variability in cloud cover . In addition, individual clouds (in particular cumulus) can be very irregular, associated with inefficient vertical overlap. It is therefore essential to understand the geometry and spatial structure of shallow cumulus (Scu) cloud fields to be able to simulate the radiative fluxes adequately. Reliable cloud population information in terms of size is also necessary for the scale-aware parameteriz…</description>
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    <item rdf:about="https://atmos.meteo.uni-koeln.de/inscape/doku.php?id=start&amp;rev=1706015630&amp;do=diff">
        <dc:format>text/html</dc:format>
        <dc:date>2024-01-23T13:13:50+00:00</dc:date>
        <dc:creator>Anonymous (anonymous@undisclosed.example.com)</dc:creator>
        <title>start</title>
        <link>https://atmos.meteo.uni-koeln.de/inscape/doku.php?id=start&amp;rev=1706015630&amp;do=diff</link>
        <description>An introduction to InScAPE

[Ray tracing volume rendering of simulated cumulus clouds at the JOYCE site on 24 June 2014]

The research group for Integrated Scale-Adaptive Parameterization and Evaluation (InScAPE) of Prof. Roel Neggers aims to develop scale-adaptive parameterizations of small-scale turbulent/convective processes and clouds for larger-scale models, and to constrain those with relevant measurements as obtained from permanent meteorological</description>
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        <dc:format>text/html</dc:format>
        <dc:date>2024-05-21T12:13:06+00:00</dc:date>
        <dc:creator>Anonymous (anonymous@undisclosed.example.com)</dc:creator>
        <title>students</title>
        <link>https://atmos.meteo.uni-koeln.de/inscape/doku.php?id=students&amp;rev=1716293586&amp;do=diff</link>
        <description>Student projects

A year in LES (AYIL): Large eddy simulation of the complete MOSAiC drift

From September 2019 to October 2020 the Polarstern Research Vessel drifted with the sea ice through the central Arctic, as part of the MOSAiC field campaign. Based on the observational data collected on the ship and by the instrumentation on the sea ice (MetCity), we performed daily Large-Eddy Simulations (LES) of the atmospheric domain surrounding the ship. The spatial and temporal resolutions were high …</description>
    </item>
    <item rdf:about="https://atmos.meteo.uni-koeln.de/inscape/doku.php?id=testbed&amp;rev=1611350494&amp;do=diff">
        <dc:format>text/html</dc:format>
        <dc:date>2021-01-22T21:21:34+00:00</dc:date>
        <dc:creator>Anonymous (anonymous@undisclosed.example.com)</dc:creator>
        <title>testbed</title>
        <link>https://atmos.meteo.uni-koeln.de/inscape/doku.php?id=testbed&amp;rev=1611350494&amp;do=diff</link>
        <description>InScAPE Parameterization Testbed

Science objectives

A parameterization testbed is an environment where model and observational datastreams come together and can easily be inter-compared. The aim is to facilitate the parameterization evaluation and development process, by confronting models with data in a structural and informed manner. While such evaluation can give confidence in the realism of a model simulation, on the other hand the models can help to gain insight into processes as they act…</description>
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    <item rdf:about="https://atmos.meteo.uni-koeln.de/inscape/doku.php?id=vacancies&amp;rev=1708549608&amp;do=diff">
        <dc:format>text/html</dc:format>
        <dc:date>2024-02-21T21:06:48+00:00</dc:date>
        <dc:creator>Anonymous (anonymous@undisclosed.example.com)</dc:creator>
        <title>vacancies</title>
        <link>https://atmos.meteo.uni-koeln.de/inscape/doku.php?id=vacancies&amp;rev=1708549608&amp;do=diff</link>
        <description>Open positions in our research group

Currently there are no open positions. 

For student projects, please refer to Student projects

----------

Past calls

🌨 Are you interested in the Arctic and meteorology?

DFG-funded Collaborative Research Centre on Arctic Amplification (</description>
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