FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4221112410> ?p ?o ?g. }

• W4221112410 abstract "&lt;div&gt; &lt;div&gt;&lt;span&gt;For the first time, we present a comparison of atmospheric transport models for Carbonyl Sulfide (COS), a promising photosynthesis tracer, within the framework of the ongoing Atmospheric Tracer Transport Model Intercomparison Project (TransCom). Seven atmospheric transport models participated in the inter-comparison experiment and provided simulations of COS mixing ratios in the troposphere over a 10-year period (2010&amp;#8211;2019), using prescribed state of the art surface fluxes for each component of the atmospheric COS budget (i.e., linked to vegetation, soil, ocean, fire and industry). The main goals of TransCom-COS are (a) to investigate the roles of the transport uncertainty and emission distribution in simulating the spatio-temporal variability of COS mixing ratio in the troposphere and (b) to assess the sensitivity of simulated tropospheric COS mixing ratio to the seasonal variability of the COS terrestrial fluxes. Models were run with the same prior emissions and without chemistry to isolate differences due to transport. Two COS flux scenarios were compared: one using a biospheric flux with a monthly time resolution and the other one using a biospheric flux with a tri-hourly time resolution. In addition, we investigated the sensitivity of the simulated concentrations to different biospheric fluxes and to indirect oceanic emissions through DMS. The modelled COS mixing ratios were assessed against observations from in situ surface stations, aircraft and ground based FTIR stations.&amp;#160;&lt;/span&gt;&lt;/div&gt; &lt;div&gt;&lt;span&gt;Using the state of the art surface fluxes for each component of the COS budget, preliminary results indicate that all transport models fail to capture the surface latitudinal distribution of COS. The COS mixing ratios are underestimated by at least 50 ppt in the tropics, pointing to a missing tropical source. In summer, the mixing ratios are overestimated by at least 50 ppt above 40N, pointing to a likely missing sink in the high northern latitudes during this period. The surface variability of COS mixing ratios is more sensitive to transport models than to a change in biospheric fluxes (two estimates based on different global Land Surface Models). Regarding the seasonal mean latitudinal profiles, the model spread is greater than 60 ppt above 40N in boreal summer and in the vicinity of anthropogenic sources. Regarding the seasonal amplitude, the model spread reaches 50 ppt at 6 sites out of 15, compared to an observed seasonal amplitude of 100 ppt. All models simulated a too late minimum by 2 to 3 months at northern sites ALT, BRW owing to likely errors in the seasonal cycle in the ocean emissions. Finally, the temporal resolution of the biospheric fluxes (monthly versus tri-hourly) has a small impact (less than 20 ppt) on the mean seasonal cycle at stations from the NOAA network.&lt;/span&gt;&lt;/div&gt; &lt;/div&gt;" @default.
• W4221112410 created "2022-04-03" @default.
• W4221112410 creator A5021466782 @default.
• W4221112410 creator A5024592114 @default.
• W4221112410 creator A5030850983 @default.
• W4221112410 creator A5032001360 @default.
• W4221112410 creator A5041708155 @default.
• W4221112410 creator A5044172237 @default.
• W4221112410 creator A5044992727 @default.
• W4221112410 creator A5050961027 @default.
• W4221112410 creator A5055249050 @default.
• W4221112410 creator A5056081169 @default.
• W4221112410 creator A5057926897 @default.
• W4221112410 creator A5061824436 @default.
• W4221112410 creator A5072273650 @default.
• W4221112410 creator A5080002210 @default.
• W4221112410 creator A5087189588 @default.
• W4221112410 date "2022-03-28" @default.
• W4221112410 modified "2023-09-29" @default.
• W4221112410 title "Simulation of atmospheric COS mixing ratio : Evaluating the impact of transport and emission distribution on COS tropospheric variability using ground-based, aircraft, and FTIR data&#160;" @default.
• W4221112410 doi "https://doi.org/10.5194/egusphere-egu22-9394" @default.
• W4221112410 hasPublicationYear "2022" @default.
• W4221112410 type Work @default.
• W4221112410 citedByCount "0" @default.
• W4221112410 crossrefType "posted-content" @default.
• W4221112410 hasAuthorship W4221112410A5021466782 @default.
• W4221112410 hasAuthorship W4221112410A5024592114 @default.
• W4221112410 hasAuthorship W4221112410A5030850983 @default.
• W4221112410 hasAuthorship W4221112410A5032001360 @default.
• W4221112410 hasAuthorship W4221112410A5041708155 @default.
• W4221112410 hasAuthorship W4221112410A5044172237 @default.
• W4221112410 hasAuthorship W4221112410A5044992727 @default.
• W4221112410 hasAuthorship W4221112410A5050961027 @default.
• W4221112410 hasAuthorship W4221112410A5055249050 @default.
• W4221112410 hasAuthorship W4221112410A5056081169 @default.
• W4221112410 hasAuthorship W4221112410A5057926897 @default.
• W4221112410 hasAuthorship W4221112410A5061824436 @default.
• W4221112410 hasAuthorship W4221112410A5072273650 @default.
• W4221112410 hasAuthorship W4221112410A5080002210 @default.
• W4221112410 hasAuthorship W4221112410A5087189588 @default.
• W4221112410 hasConcept C121332964 @default.
• W4221112410 hasConcept C138777275 @default.
• W4221112410 hasConcept C153294291 @default.
• W4221112410 hasConcept C178790620 @default.
• W4221112410 hasConcept C18459110 @default.
• W4221112410 hasConcept C185544564 @default.
• W4221112410 hasConcept C185592680 @default.
• W4221112410 hasConcept C2777517185 @default.
• W4221112410 hasConcept C2778798282 @default.
• W4221112410 hasConcept C2778863792 @default.
• W4221112410 hasConcept C39432304 @default.
• W4221112410 hasConcept C49999975 @default.
• W4221112410 hasConcept C508106653 @default.
• W4221112410 hasConcept C518881349 @default.
• W4221112410 hasConcept C62520636 @default.
• W4221112410 hasConcept C68709404 @default.
• W4221112410 hasConcept C9075549 @default.
• W4221112410 hasConcept C91586092 @default.
• W4221112410 hasConceptScore W4221112410C121332964 @default.
• W4221112410 hasConceptScore W4221112410C138777275 @default.
• W4221112410 hasConceptScore W4221112410C153294291 @default.
• W4221112410 hasConceptScore W4221112410C178790620 @default.
• W4221112410 hasConceptScore W4221112410C18459110 @default.
• W4221112410 hasConceptScore W4221112410C185544564 @default.
• W4221112410 hasConceptScore W4221112410C185592680 @default.
• W4221112410 hasConceptScore W4221112410C2777517185 @default.
• W4221112410 hasConceptScore W4221112410C2778798282 @default.
• W4221112410 hasConceptScore W4221112410C2778863792 @default.
• W4221112410 hasConceptScore W4221112410C39432304 @default.
• W4221112410 hasConceptScore W4221112410C49999975 @default.
• W4221112410 hasConceptScore W4221112410C508106653 @default.
• W4221112410 hasConceptScore W4221112410C518881349 @default.
• W4221112410 hasConceptScore W4221112410C62520636 @default.
• W4221112410 hasConceptScore W4221112410C68709404 @default.
• W4221112410 hasConceptScore W4221112410C9075549 @default.
• W4221112410 hasConceptScore W4221112410C91586092 @default.
• W4221112410 hasLocation W42211124101 @default.
• W4221112410 hasOpenAccess W4221112410 @default.
• W4221112410 hasPrimaryLocation W42211124101 @default.
• W4221112410 hasRelatedWork W1584734414 @default.
• W4221112410 hasRelatedWork W1973289087 @default.
• W4221112410 hasRelatedWork W2056551787 @default.
• W4221112410 hasRelatedWork W2115907986 @default.
• W4221112410 hasRelatedWork W2153989975 @default.
• W4221112410 hasRelatedWork W2594153921 @default.
• W4221112410 hasRelatedWork W2761189297 @default.
• W4221112410 hasRelatedWork W2955234884 @default.
• W4221112410 hasRelatedWork W3007899655 @default.
• W4221112410 hasRelatedWork W4221112410 @default.
• W4221112410 isParatext "false" @default.
• W4221112410 isRetracted "false" @default.
• W4221112410 workType "article" @default.