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Sökning: onr:"swepub:oai:lup.lub.lu.se:312d04ac-1711-429c-a180-837bd9eabf2d" > Modelling CO2 weath...

Modelling CO2 weather-why horizontal resolution matters

Agustí-Panareda, Anna (författare)
European Centre for Medium-range Weather Forecasts
Diamantakis, Michail (författare)
European Centre for Medium-range Weather Forecasts
Massart, Sébastien (författare)
European Centre for Medium-range Weather Forecasts
visa fler...
Chevallier, Frédéric (författare)
Versailles Saint-Quentin-en-Yvelines University
Muñoz-Sabater, Joaquín (författare)
European Centre for Medium-range Weather Forecasts
Barré, Jérôme (författare)
European Centre for Medium-range Weather Forecasts
Curcoll, Roger (författare)
Autonomous University of Barcelona
Engelen, Richard (författare)
European Centre for Medium-range Weather Forecasts
Langerock, Bavo (författare)
Belgian Institute for Space Aeronomy
Law, Rachel M. (författare)
CSIRO Oceans and Atmosphere, Canberra
Loh, Zoë (författare)
CSIRO Oceans and Atmosphere, Canberra
Morguí, Josep Anton (författare)
Autonomous University of Barcelona
Parrington, Mark (författare)
European Centre for Medium-range Weather Forecasts
Peuch, Vincent Henri (författare)
European Centre for Medium-range Weather Forecasts
Ramonet, Michel (författare)
Versailles Saint-Quentin-en-Yvelines University
Roehl, Coleen (författare)
California Institute of Technology
Vermeulen, Alex T. (författare)
Lund University,Lunds universitet,Institutionen för naturgeografi och ekosystemvetenskap,Naturvetenskapliga fakulteten,Dept of Physical Geography and Ecosystem Science,Faculty of Science,ICOS ERIC Carbon Portal
Warneke, Thorsten (författare)
University of Bremen
Wunch, Debra (författare)
University of Toronto
visa färre...
 (creator_code:org_t)
2019-06-04
2019
Engelska 30 s.
Ingår i: Atmospheric Chemistry and Physics. - : Copernicus GmbH. - 1680-7316 .- 1680-7324. ; 19:11, s. 7347-7376
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
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  • Climate change mitigation efforts require information on the current greenhouse gas atmospheric concentrations and their sources and sinks. Carbon dioxide (CO2) is the most abundant anthropogenic greenhouse gas. Its variability in the atmosphere is modulated by the synergy between weather and CO2 surface fluxes, often referred to as CO2 weather. It is interpreted with the help of global or regional numerical transport models, with horizontal resolutions ranging from a few hundreds of kilometres to a few kilometres. Changes in the model horizontal resolution affect not only atmospheric transport but also the representation of topography and surface CO2 fluxes. This paper assesses the impact of horizontal resolution on the simulated atmospheric CO2 variability with a numerical weather prediction model. The simulations are performed using the Copernicus Atmosphere Monitoring Service (CAMS) CO2 forecasting system at different resolutions from 9 to 80 km and are evaluated using in situ atmospheric surface measurements and atmospheric column-mean observations of CO2, as well as radiosonde and SYNOP observations of the winds. The results indicate that both diurnal and day-to-day variability of atmospheric CO2 are generally better represented at high resolution, as shown by a reduction in the errors in simulated wind and CO2. Mountain stations display the largest improvements at high resolution as they directly benefit from the more realistic orography. In addition, the CO2 spatial gradients are generally improved with increasing resolution for both stations near the surface and those observing the total column, as the overall inter-station error is also reduced in magnitude. However, close to emission hotspots, the high resolution can also lead to a deterioration of the simulation skill, highlighting uncertainties in the high-resolution fluxes that are more diffuse at lower resolutions. We conclude that increasing horizontal resolution matters for modelling CO2 weather because it has the potential to bring together improvements in the surface representation of both winds and CO2 fluxes, as well as an expected reduction in numerical errors of transport. Modelling applications like atmospheric inversion systems to estimate surface fluxes will only be able to benefit fully from upgrades in horizontal resolution if the topography, winds and prior flux distribution are also upgraded accordingly. It is clear from the results that an additional increase in resolution might reduce errors even further. However, the horizontal resolution sensitivity tests indicate that the change in the CO2 and wind modelling error with resolution is not linear, making it difficult to quantify the improvement beyond the tested resolutions. Finally, we show that the high-resolution simulations are useful for the assessment of the small-scale variability of CO2 which cannot be represented in coarser-resolution models. These representativeness errors need to be considered when assimilating in situ data and high-resolution satellite data such as Greenhouse gases Observing Satellite (GOSAT), Orbiting Carbon Observatory-2 (OCO-2), the Chinese Carbon Dioxide Observation Satellite Mission (TanSat) and future missions such as the Geostationary Carbon Observatory (GeoCarb) and the Sentinel satellite constellation for CO2. For these reasons, the high-resolution CO2 simulations provided by the CAMS in real time can be useful to estimate such small-scale variability in real time, as well as providing boundary conditions for regional modelling studies and supporting field experiments.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Meteorologi och atmosfärforskning (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Meteorology and Atmospheric Sciences (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Klimatforskning (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Climate Research (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Environmental Sciences (hsv//eng)

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