Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

Simulation setup for atmospheric CH4 concentrations in the ICON-ART Limited Area Mode

View through CrossRef
An experimental setup within ICON (ICOsahedral Non-hydrostatic)-ART (Aerosols and Reactive Trace gases) has been  carried out to simulate the atmospheric CH4 concentration over Europe during the investigation period from 01 May 2018 to 30 June 2018.Modelling CH4 in the Limited Area Mode (Europe, 6.5 x 6.5 km), the model requires as accurate as possible initial and boundary atmospheric conditions as well as spatially highly resolved emissions. Temporal resolved emissions are to be included in the next step. While the intial data denote here the state of the atmosphere (meteorological and CH4 concentration fields) at the start of the model run, the boundary conditions shall denote the data in the lateral boundary zone where the model is forced by the meteorological and CH4 concentration data outside the domain. We have used DWD's operational numerical weather prediction output as meteorological boundary conditions. The Copernicus Atmosphere Monitoring Service (CAMS) provides the necessary initial and boundary CH4 data, which are made applicable  for the ICON-ART before the model run in Limited Area Mode. The regional CH4 emissions for Europe have been  provided by TNO and are processed with the ART module.  Since CAMS uses a vertical coordinate of a hybrid sigma-pressure system, the data had been horizontally and vertically interpolated to the height based SLEVE coordinate system of ICON. The sectorial CH4 emissions for Europe and for Germany were mapped separately to the target ICON grid by preprocessing the corresponding reported methane emissions of various sectors (resulting in 36 distinct methane variables in the model). The 50 largest point emissions from each sector are treated separately, smaller point emissions are treated together with the area emissions.To run a hourly experimental setup for two month the Basic Cycling environment (BACY) tool was used. The fields for meteorological parameters were initialized daily by using the DWD's operational data, while the atmospheric CH4 concentrations are taken from the previous ICON-ART CH4 simulation results (e.g., the 24 h CH4 forecast from the previous day). Then, the merged concentration fields for meterological conditions and atmospheric methane are used as “DWD first guess”, which served for a daily start of the simulation process in the ICON-ART Limited Area Mode. In order to compare the model results and measurements from the Integrated Carbon Observation System (ICOS) stations, the model equivalents have been extracted at the locations of the  ICOS montoring stations  using the “Model Equivalent Calculator”.In this work, the ICON-ART CH4 simulation setup for Limited Area Mode (Europe) was forced by ICON meteorology and CAMS CH4 boundary data and had been started daily by the merged “DWD first guess”. These are shown to be a useful method to simulate the CH4 atmospheric concentrations at the regional scale.
Title: Simulation setup for atmospheric CH4 concentrations in the ICON-ART Limited Area Mode
Description:
An experimental setup within ICON (ICOsahedral Non-hydrostatic)-ART (Aerosols and Reactive Trace gases) has been  carried out to simulate the atmospheric CH4 concentration over Europe during the investigation period from 01 May 2018 to 30 June 2018.
Modelling CH4 in the Limited Area Mode (Europe, 6.
5 x 6.
5 km), the model requires as accurate as possible initial and boundary atmospheric conditions as well as spatially highly resolved emissions.
Temporal resolved emissions are to be included in the next step.
While the intial data denote here the state of the atmosphere (meteorological and CH4 concentration fields) at the start of the model run, the boundary conditions shall denote the data in the lateral boundary zone where the model is forced by the meteorological and CH4 concentration data outside the domain.
We have used DWD's operational numerical weather prediction output as meteorological boundary conditions.
The Copernicus Atmosphere Monitoring Service (CAMS) provides the necessary initial and boundary CH4 data, which are made applicable  for the ICON-ART before the model run in Limited Area Mode.
The regional CH4 emissions for Europe have been  provided by TNO and are processed with the ART module.
 Since CAMS uses a vertical coordinate of a hybrid sigma-pressure system, the data had been horizontally and vertically interpolated to the height based SLEVE coordinate system of ICON.
The sectorial CH4 emissions for Europe and for Germany were mapped separately to the target ICON grid by preprocessing the corresponding reported methane emissions of various sectors (resulting in 36 distinct methane variables in the model).
The 50 largest point emissions from each sector are treated separately, smaller point emissions are treated together with the area emissions.
To run a hourly experimental setup for two month the Basic Cycling environment (BACY) tool was used.
The fields for meteorological parameters were initialized daily by using the DWD's operational data, while the atmospheric CH4 concentrations are taken from the previous ICON-ART CH4 simulation results (e.
g.
, the 24 h CH4 forecast from the previous day).
Then, the merged concentration fields for meterological conditions and atmospheric methane are used as “DWD first guess”, which served for a daily start of the simulation process in the ICON-ART Limited Area Mode.
In order to compare the model results and measurements from the Integrated Carbon Observation System (ICOS) stations, the model equivalents have been extracted at the locations of the  ICOS montoring stations  using the “Model Equivalent Calculator”.
In this work, the ICON-ART CH4 simulation setup for Limited Area Mode (Europe) was forced by ICON meteorology and CAMS CH4 boundary data and had been started daily by the merged “DWD first guess”.
These are shown to be a useful method to simulate the CH4 atmospheric concentrations at the regional scale.

Related Results

Isotopic characterization of methane emissions in Malaga, Spain
Isotopic characterization of methane emissions in Malaga, Spain
The reduction of methane emissions from energy, agriculture, and waste sectors presents a significant opportunity for making near-term strides in climate mitigation. To accomplish ...
Gridded maps of geological methane emissions and their isotopic signature
Gridded maps of geological methane emissions and their isotopic signature
Abstract. Methane (CH4) is a powerful greenhouse gas, whose natural and anthropogenic emissions contribute ~20% to global radiative forcing. Its atmospheric budget (sources and sin...
Sensitivities of simulated atmospheric CH4 concentrations in the ICON-ART Limited Area Mode
Sensitivities of simulated atmospheric CH4 concentrations in the ICON-ART Limited Area Mode
<p>We conducted CH<sub>4 </sub>simulations for Europe by using the ICON (<strong>ICO</strong>sahedral <...
Methane Flux Dynamics in a California Oak Savanna
Methane Flux Dynamics in a California Oak Savanna
Methane (CH4) is a potent greenhouse gas, yet the role of trees in the global CH4 budget remains uncertain. While some studies report CH4 emissions from wetland and certain upland ...
Soil Methanotrophy Model (MeMo v1.0): a process-based model to quantify global uptake of atmospheric methane by soil
Soil Methanotrophy Model (MeMo v1.0): a process-based model to quantify global uptake of atmospheric methane by soil
Abstract. Soil bacteria known as methanotrophs are the sole biological sink for atmospheric methane (CH4), a potent greenhouse gas that is responsible for ∼ 20 % of the human-drive...
Variability of tree methane emissions across regions of the Amazon rainforest
Variability of tree methane emissions across regions of the Amazon rainforest
Trees are recently understood to emit large quantities of CH4 through their stems, particularly in tropical wetland environments. There are still large uncertainties of the process...
Elevated Methane in Massachusetts and Rhode Island Homes Using Fracked Gas
Elevated Methane in Massachusetts and Rhode Island Homes Using Fracked Gas
We surveyed 197 Massachusetts and Rhode Island houses ranging in building style and age to test whether homes served by fracked gas have higher indoor methane concentrations ([CH4]...
Effects of electron acceptors on CH4 emission in alpine wetlands
Effects of electron acceptors on CH4 emission in alpine wetlands
Alpine wetlands are an important source of methane (CH4) and play a key role in the global carbon cycle. Their CH4 emissions largely depend on microbial CH4 production and oxidatio...

Back to Top