This project envelops different activities using the multi-resolution Finite Element Sea Ice-Ocean Model (FESOM) for climate studies. FESOM is used primarily at Climate Sciences division of AWI and is
HD(CP)2 – High definition clouds and precipitation for advancing climate prediction is a framework project funded by BMBF. The general target of the project is to advance the understanding of cloud formation
StratoClim
is an EU FP7 project over the time period 1.12.2013 - 30.11.2018, http://www.stratoclim.org/ . The aim of StratoClim is to improve climate projections by (1) developing the scientific basis
Stratosphere in the Earth System The role of gravity waves for the stratospheric circulation and its variability is the primary objective of this project. To gain a better understanding of the interaction
Die Reaktion eines Klimamodells auf einen veranderten externen Antrieb hängt nicht nur von der Darstellung dieses Antriebs ab, sondern auch von der Beschreibung interner Wechselwirkungen zwischen sehr
In addition to satellite observations yielding SSH- and SST-information, which also in the Institute of Oceanography of the University of Hamburg (IfM) has intensively been used to validate and to improve
The project bm0081 has the following objectives:
a) Impact of model resolution (up to T106 horizontally and up to 39 layers) on the
systematic errors of the model. Experiments with prescribed observed
The ICON dynamical core is a new development initiated by the Max Planck Institute for Meteorology (MPI-M) and the Deutscher Wetterdienst (DWD). This dynamical core will combine several properties, which
Ocean Model Development Ocean models are an important part of all earth system models. Like any other model types they need to be tested and improved. At the MPI two ocean/sea ice models (LSG and HOPE)
The Horizon 2020 project BINGO: Bringing INnovation to onGOing water management - a better future under climate change (2015-2019) aims at providing practical knowledge and tools to end users, water managers,
HD(CP)² – High definition clouds and precipitation for advancing climate prediction ‐ is a framework project funded by BMBF, it focuses on the question as to whether very high resolution models, integrated
MiKlip (Mittelfristige Klimaprognose) is a BMBF funded project on decadal climate prediction. For more information on MiKlip, visit the project website https://www.fona-miklip.de/ The aim of the project
The JSBACH (Jena-Scheme for Biosphere-Atmosphere Coupling in Hamburg) and TRACES (Trace Gases and Aerosol Cycles in the Earth System) project aims at the integration of climate and biogeochemistry model
The main goal of Module B of MiKLIP is to improve the understanding of processes leading to decadal climate variability. Several of these have already been included in climate models, but their importance
Data set provides the model results of ECHAM5-HAM when injecting SO2
with different injection strength and areas into the stratosphere.
see also Niemeier and Schmidt, Changing transport processes in
In this study we conducted four simulations with JSBACH-SPITFIRE using different kinds of temporal averages of the cloud-to-ground lightning forcing data, while applying the same meteorological forcing.
High definition clouds and precipitation for advancing climate prediction (HD(CP)2) is a framework project funded by BMBF. The general target of the project is to advance the understanding of cloud formation
Externally forced simulations for the climate of the late-Holocene (2-3ka BP - present), and future climate, shall be undertaken, using either the ECHO-G or ECHAM5/MPI-OM AOGCMs. Existing simulations
Modelling of the coupled system ocean / atmosphere / sea ice We shall study the dynamics of the coupled system ocean / atmosphere / sea ice by conducting numerical simulations. The experiments will be
These are the primary data of the paper "Sensitivity of Simulated Meospsheric Transport of Nitrogen Oxides to Parameterized Gravity Waves" written by K. Meraner, H. Schmidt, E. Manzini, B. Funke and A.
This project is a part of BMBF-project CADY(Central Asia Dynamics). In this project, palaeoclimate simulations of different durations will be carried out for selected time periods.. The combination of
Forecasting the development, track and intensity of hurricanes requires both, a high model resolution to capture all the multi-scale interactions, prerequisite for the development of the initial Tropical
Permafrost or perennially frozen ground is an important part of the terrestrial cryosphere; roughly one quarter of Earth s land surface is underlain by permafrost. The impact of the currently observed
The soil moisture initialization experiment is composed of two sets of simulations. The first set consists of one reference simulation (REF) for the period 1995--2008. It's initial states were taken from
CMIP5 Klimasimulationen und deren Regionalisierung Summaries: see summaries of related entries: - CORDEX Antriebsdaten - EUR-11 CCLM Evaluierungsexperiment - CMIP5 archive data based on MPI-ESM-LR/-P/-MR
Record disasters such as earthquakes, hurricanes (or typhoons), tsunamis, widespread flooding and pollution, droughts, extremes of snowfalls and temperatures - all of which are associated with devastating
MiKlip/VECAP: VErification, Calibration and Assessment of Predictability of medium-range climate predicions using satellite data (bb0763)
VeCAP is a contribution to the BMBF research programme MiKlip
Significant amounts of ozone have stratospheric origin and are transported to the troposphere along deep tropopause folds. Since they influence the long-term trend of tropospheric ozone, it is therefore
Simulations with the MPI-ESM coupled via energy balance calculation with the ice sheet model PISM. Simulations following four scenarios: a) pre industrial control run (piControl_r1i1p1-P07) b) abrupt
Model output from experiments with the regionally coupled model MPIOM/REMO for the Arctic. External forcing is used ECHAM5 from CMIP3 experiments (for the experiments 437,438,600,601,605,700 and 800).
Model output from experiments with the regionally coupled model MPIOM/REMO for the Arctic. External forcing is used from NCEP/NCAR reanalysis data (for the experiments 436 and 602) and from ECHAM5 from
Data are results of dynamical downscaling of NCEP/NCAR reanalysis, ECHAM5/MPIOM 20th century run and A1B scenario run for the North Atlantic and North European shelves. For the downscaling the global ocean-sea
The TFO research project focuses on the Okavango basin with its variety of savannah woodlands and wetland ecosystems linked by the central lifeline of the Okavango river. The region is a global hot-spot
The main objectives of "Aerosol and Climate" are: i) To assess the direct and indirect climate effect of aerosols and quantify and reduce several of the associated main uncertainties using climate models.
From 2006 to 2011 the MPI-M established the "Super Volcano" (SV) project as one of its crosscutting science projects. Detailed information about the project can be obtained from the project web page (
Sensitivity studies on the production of marine DMS under rising CO2 with MPI-ESM and ECHAM5/HAM2
Results published in Nature Climate Change, doi:1C.1C38/nclimate1981, 2C13.
Six K.D., Kloster S., Ilyina
Project: MiKlip-VESPA Experiments: idealized simulations under constant pre-industrial orbital and GHG conditions, sea surface temperature anomaly pattern from Schubert et al. 2009 corresponding to warm
The climate of the Last Glacial showed much higher variability than the present day climate. Some of this larger variability is due to the interaction of the larger ice sheets with the other components
A global atmospheric General Circulation Model (Echam5-wiso) with capability of predicting 18O (a Paleo-environmental Proxies) has been performed for a topography sensitivity analysis. The Tibet plateau
- project name and number ProSECCO, bb0286 - additional useful project information ProSECCO was funded by DFG as part of the Priority Project CAWSES (SPP 1176)
GCM experiments with COSMOS-ASO for the DFG Project (FOR 1070):
Understanding Cenozoic Climate Cooling: The Role of the Hydrological Cycle, the Carbon Cycle, and Vegetation Changes
Experimental design: