The CAMS reanalysis of atmospheric composition
<p>The Copernicus Atmosphere Monitoring Service (CAMS) reanalysis is the latest global reanalysis dataset of atmospheric composition produced by the European Centre for Medium-Range Weather Forecasts (ECMWF), consisting of three-dimensional time-consistent atmospheric composition fields, inclu...
| الحاوية / القاعدة: | Atmospheric Chemistry and Physics |
|---|---|
| المؤلفون الرئيسيون: | , , , , , , , , , , , , , , , , , , , |
| التنسيق: | مقال |
| اللغة: | الإنجليزية |
| منشور في: |
Copernicus Publications
2019-03-01
|
| الموضوعات: | |
| الوصول للمادة أونلاين: | https://www.atmos-chem-phys.net/19/3515/2019/acp-19-3515-2019.pdf |
| _version_ | 1849359193289523200 |
|---|---|
| author | A. Inness M. Ades A. Agustí-Panareda J. Barré A. Benedictow A.-M. Blechschmidt J. J. Dominguez R. Engelen H. Eskes J. Flemming V. Huijnen L. Jones Z. Kipling S. Massart M. Parrington V.-H. Peuch M. Razinger S. Remy M. Schulz M. Suttie |
| author_facet | A. Inness M. Ades A. Agustí-Panareda J. Barré A. Benedictow A.-M. Blechschmidt J. J. Dominguez R. Engelen H. Eskes J. Flemming V. Huijnen L. Jones Z. Kipling S. Massart M. Parrington V.-H. Peuch M. Razinger S. Remy M. Schulz M. Suttie |
| author_sort | A. Inness |
| collection | DOAJ |
| container_title | Atmospheric Chemistry and Physics |
| description | <p>The Copernicus Atmosphere Monitoring Service (CAMS)
reanalysis is the latest global reanalysis dataset of atmospheric
composition produced by the European Centre for Medium-Range Weather
Forecasts (ECMWF), consisting of three-dimensional time-consistent atmospheric
composition fields, including aerosols and chemical species. The dataset
currently covers the period 2003–2016 and will be extended in the future by
adding 1 year each year. A reanalysis for greenhouse gases is being
produced separately. The CAMS reanalysis builds on the experience gained
during the production of the earlier Monitoring Atmospheric Composition and
Climate (MACC) reanalysis and CAMS interim reanalysis. Satellite retrievals
of total column CO; tropospheric column <span class="inline-formula">NO<sub>2</sub></span>; aerosol optical depth (AOD); and
total column, partial column and profile ozone retrievals were assimilated
for the CAMS reanalysis with ECMWF's Integrated Forecasting System. The new
reanalysis has an increased horizontal resolution of about 80 km and
provides more chemical species at a better temporal resolution (3-hourly
analysis fields, 3-hourly forecast fields and hourly surface forecast
fields) than the previously produced CAMS interim reanalysis. The CAMS
reanalysis has smaller biases compared with most of the independent ozone,
carbon monoxide, nitrogen dioxide and aerosol optical depth observations
used for validation in this paper than the previous two reanalyses and is
much improved and more consistent in time, especially compared to the MACC
reanalysis. The CAMS reanalysis is a dataset that can be used to compute
climatologies, study trends, evaluate models, benchmark other reanalyses or
serve as boundary conditions for regional models for past periods.</p> |
| format | Article |
| id | doaj-art-e8254132a6eb43b4881d44cc685df7df |
| institution | Directory of Open Access Journals |
| issn | 1680-7316 1680-7324 |
| language | English |
| publishDate | 2019-03-01 |
| publisher | Copernicus Publications |
| record_format | Article |
| spelling | doaj-art-e8254132a6eb43b4881d44cc685df7df2025-08-28T15:28:20ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242019-03-01193515355610.5194/acp-19-3515-2019The CAMS reanalysis of atmospheric compositionA. Inness0M. Ades1A. Agustí-Panareda2J. Barré3A. Benedictow4A.-M. Blechschmidt5J. J. Dominguez6R. Engelen7H. Eskes8J. Flemming9V. Huijnen10L. Jones11Z. Kipling12S. Massart13M. Parrington14V.-H. Peuch15M. Razinger16S. Remy17M. Schulz18M. Suttie19ECMWF, Shinfield Park, Reading, RG2 9AX, UKECMWF, Shinfield Park, Reading, RG2 9AX, UKECMWF, Shinfield Park, Reading, RG2 9AX, UKECMWF, Shinfield Park, Reading, RG2 9AX, UKNorwegian Meteorological Institute, Postboks 43 Blindern, 0313 Oslo, NorwayInstitute of Environmental Physics, University of Bremen, Bremen, GermanyECMWF, Shinfield Park, Reading, RG2 9AX, UKECMWF, Shinfield Park, Reading, RG2 9AX, UKRoyal Netherlands Meteorological Institute, De Bilt, the NetherlandsECMWF, Shinfield Park, Reading, RG2 9AX, UKRoyal Netherlands Meteorological Institute, De Bilt, the NetherlandsECMWF, Shinfield Park, Reading, RG2 9AX, UKECMWF, Shinfield Park, Reading, RG2 9AX, UKECMWF, Shinfield Park, Reading, RG2 9AX, UKECMWF, Shinfield Park, Reading, RG2 9AX, UKECMWF, Shinfield Park, Reading, RG2 9AX, UKECMWF, Shinfield Park, Reading, RG2 9AX, UKIPSL, CNRS/UPMC, Paris, FranceNorwegian Meteorological Institute, Postboks 43 Blindern, 0313 Oslo, NorwayECMWF, Shinfield Park, Reading, RG2 9AX, UK<p>The Copernicus Atmosphere Monitoring Service (CAMS) reanalysis is the latest global reanalysis dataset of atmospheric composition produced by the European Centre for Medium-Range Weather Forecasts (ECMWF), consisting of three-dimensional time-consistent atmospheric composition fields, including aerosols and chemical species. The dataset currently covers the period 2003–2016 and will be extended in the future by adding 1 year each year. A reanalysis for greenhouse gases is being produced separately. The CAMS reanalysis builds on the experience gained during the production of the earlier Monitoring Atmospheric Composition and Climate (MACC) reanalysis and CAMS interim reanalysis. Satellite retrievals of total column CO; tropospheric column <span class="inline-formula">NO<sub>2</sub></span>; aerosol optical depth (AOD); and total column, partial column and profile ozone retrievals were assimilated for the CAMS reanalysis with ECMWF's Integrated Forecasting System. The new reanalysis has an increased horizontal resolution of about 80 km and provides more chemical species at a better temporal resolution (3-hourly analysis fields, 3-hourly forecast fields and hourly surface forecast fields) than the previously produced CAMS interim reanalysis. The CAMS reanalysis has smaller biases compared with most of the independent ozone, carbon monoxide, nitrogen dioxide and aerosol optical depth observations used for validation in this paper than the previous two reanalyses and is much improved and more consistent in time, especially compared to the MACC reanalysis. The CAMS reanalysis is a dataset that can be used to compute climatologies, study trends, evaluate models, benchmark other reanalyses or serve as boundary conditions for regional models for past periods.</p>https://www.atmos-chem-phys.net/19/3515/2019/acp-19-3515-2019.pdfopen climate campaign |
| spellingShingle | A. Inness M. Ades A. Agustí-Panareda J. Barré A. Benedictow A.-M. Blechschmidt J. J. Dominguez R. Engelen H. Eskes J. Flemming V. Huijnen L. Jones Z. Kipling S. Massart M. Parrington V.-H. Peuch M. Razinger S. Remy M. Schulz M. Suttie The CAMS reanalysis of atmospheric composition open climate campaign |
| title | The CAMS reanalysis of atmospheric composition |
| title_full | The CAMS reanalysis of atmospheric composition |
| title_fullStr | The CAMS reanalysis of atmospheric composition |
| title_full_unstemmed | The CAMS reanalysis of atmospheric composition |
| title_short | The CAMS reanalysis of atmospheric composition |
| title_sort | cams reanalysis of atmospheric composition |
| topic | open climate campaign |
| url | https://www.atmos-chem-phys.net/19/3515/2019/acp-19-3515-2019.pdf |
| work_keys_str_mv | AT ainness thecamsreanalysisofatmosphericcomposition AT mades thecamsreanalysisofatmosphericcomposition AT aagustipanareda thecamsreanalysisofatmosphericcomposition AT jbarre thecamsreanalysisofatmosphericcomposition AT abenedictow thecamsreanalysisofatmosphericcomposition AT amblechschmidt thecamsreanalysisofatmosphericcomposition AT jjdominguez thecamsreanalysisofatmosphericcomposition AT rengelen thecamsreanalysisofatmosphericcomposition AT heskes thecamsreanalysisofatmosphericcomposition AT jflemming thecamsreanalysisofatmosphericcomposition AT vhuijnen thecamsreanalysisofatmosphericcomposition AT ljones thecamsreanalysisofatmosphericcomposition AT zkipling thecamsreanalysisofatmosphericcomposition AT smassart thecamsreanalysisofatmosphericcomposition AT mparrington thecamsreanalysisofatmosphericcomposition AT vhpeuch thecamsreanalysisofatmosphericcomposition AT mrazinger thecamsreanalysisofatmosphericcomposition AT sremy thecamsreanalysisofatmosphericcomposition AT mschulz thecamsreanalysisofatmosphericcomposition AT msuttie thecamsreanalysisofatmosphericcomposition AT ainness camsreanalysisofatmosphericcomposition AT mades camsreanalysisofatmosphericcomposition AT aagustipanareda camsreanalysisofatmosphericcomposition AT jbarre camsreanalysisofatmosphericcomposition AT abenedictow camsreanalysisofatmosphericcomposition AT amblechschmidt camsreanalysisofatmosphericcomposition AT jjdominguez camsreanalysisofatmosphericcomposition AT rengelen camsreanalysisofatmosphericcomposition AT heskes camsreanalysisofatmosphericcomposition AT jflemming camsreanalysisofatmosphericcomposition AT vhuijnen camsreanalysisofatmosphericcomposition AT ljones camsreanalysisofatmosphericcomposition AT zkipling camsreanalysisofatmosphericcomposition AT smassart camsreanalysisofatmosphericcomposition AT mparrington camsreanalysisofatmosphericcomposition AT vhpeuch camsreanalysisofatmosphericcomposition AT mrazinger camsreanalysisofatmosphericcomposition AT sremy camsreanalysisofatmosphericcomposition AT mschulz camsreanalysisofatmosphericcomposition AT msuttie camsreanalysisofatmosphericcomposition |