FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2509155656> ?p ?o ?g. }

• W2509155656 abstract "Abstract. The impact of a convection permitting (CP) northern hemisphere latitude-belt simulation with the Weather Research and Forecasting (WRF) model was investigated during the July and August 2013. For this application, the WRF model together with the NOAH land-surface model (LSM) was applied at two different horizontal resolutions, 0.03° (HIRES) and 0.12° (LOWRES). The set-up as a latitude-belt domain avoids disturbances that originate from the western and eastern boundaries and therefore allows to study the impact of model resolution and physical parameterizations on the results. Both simulations were forced by ECMWF operational analysis data at the northern and southern domain boundaries and the high-resolution Operational Sea Surface Temperature and Sea Ice Analysis (OSTIA) data at the sea surface. The simulations are compared to the operational ECMWF analysis for the representation of large scale features. To compare the simulated precipitation, the operational ECMWF forecast, the CPC MORPHing (CMORPH), and the ENSEMBLES gridded observation precipitation data set (E-OBS) were used. Compared to the operational high-resolution ECMWF analysis, both simulations are able to capture the large scale circulation pattern though the strength of the Pacific high is considerably overestimated in the LOWRES simulation. Major differences between ECMWF and WRF occur during July 2013 when the lower resolution simulation shows a significant negative bias over the North Atlantic which is not observed in the CP simulation. The analysis indicates deficiencies in the applied combinations of cloud microphysics and convection parametrization on the coarser grid scale in subpolar regions. The overall representation of the 500 hPa geopotential height surface is also improved by the CP simulation compared to the LOWRES simulation apart across Newfoundland where the geopotential height is higher than in the LOWRES simulation due to a northward shift of the location of the Atlantic high pressure system. Both simulations show higher wind speeds in the boundary layer by about 1.5 m s−1 compared to the the ECMWF analysis. Due to the higher surface evaporation, this results in a moist bias of 0.5 g kg−1 at 925 hPa in the planetary boundary layer compared to the ECMWF analysis. Major differences between ECMWF and WRF occur in the simulation of the 2-m temperatures over the Asian desert and steppe regions. They are significantly higher in WRF by about 5 K both during day- and night-time presumably as a result of different soil hydraulic parameters used in the NOAH land surface model for steppe regions. The precipitation of the HIRES simulation shows a better spatial agreement with CMORPH especially over mountainous terrain. The overall bias reduces from 80 mm at the coarser resolution to 50 mm in the HIRES simulation and the root mean square error is reduced by about 35 % when compared to the CMORPH precipitation analysis. The precipitation distribution agrees much better with the CMORPH data than the LOWRES simulation which tends to overestimate precipitation, mainly caused by the convection parametrization. Especially over Europe the CP resolution reduces the precipitation bias by about 30 % to 20 mm as a result of a better terrain representation and due to the avoidance of the convection parameterization." @default.
• W2509155656 created "2016-09-16" @default.
• W2509155656 creator A5000347460 @default.
• W2509155656 creator A5015466293 @default.
• W2509155656 creator A5026657301 @default.
• W2509155656 creator A5032267791 @default.
• W2509155656 date "2016-08-29" @default.
• W2509155656 modified "2023-09-25" @default.
• W2509155656 title "Continuous high resolution mid-latitude belt simulations for July–August 2013 with WRF" @default.
• W2509155656 doi "https://doi.org/10.5194/gmd-2016-195" @default.
• W2509155656 hasPublicationYear "2016" @default.
• W2509155656 type Work @default.
• W2509155656 sameAs 2509155656 @default.
• W2509155656 citedByCount "0" @default.
• W2509155656 crossrefType "posted-content" @default.
• W2509155656 hasAuthorship W2509155656A5000347460 @default.
• W2509155656 hasAuthorship W2509155656A5015466293 @default.
• W2509155656 hasAuthorship W2509155656A5026657301 @default.
• W2509155656 hasAuthorship W2509155656A5032267791 @default.
• W2509155656 hasBestOaLocation W25091556561 @default.
• W2509155656 hasConcept C122523270 @default.
• W2509155656 hasConcept C127313418 @default.
• W2509155656 hasConcept C13280743 @default.
• W2509155656 hasConcept C133204551 @default.
• W2509155656 hasConcept C153294291 @default.
• W2509155656 hasConcept C205649164 @default.
• W2509155656 hasConcept C39432304 @default.
• W2509155656 hasConcept C49204034 @default.
• W2509155656 hasConcept C91586092 @default.
• W2509155656 hasConceptScore W2509155656C122523270 @default.
• W2509155656 hasConceptScore W2509155656C127313418 @default.
• W2509155656 hasConceptScore W2509155656C13280743 @default.
• W2509155656 hasConceptScore W2509155656C133204551 @default.
• W2509155656 hasConceptScore W2509155656C153294291 @default.
• W2509155656 hasConceptScore W2509155656C205649164 @default.
• W2509155656 hasConceptScore W2509155656C39432304 @default.
• W2509155656 hasConceptScore W2509155656C49204034 @default.
• W2509155656 hasConceptScore W2509155656C91586092 @default.
• W2509155656 hasLocation W25091556561 @default.
• W2509155656 hasLocation W25091556562 @default.
• W2509155656 hasOpenAccess W2509155656 @default.
• W2509155656 hasPrimaryLocation W25091556561 @default.
• W2509155656 hasRelatedWork W132815485 @default.
• W2509155656 hasRelatedWork W1993414561 @default.
• W2509155656 hasRelatedWork W2270621750 @default.
• W2509155656 hasRelatedWork W2351522597 @default.
• W2509155656 hasRelatedWork W2550280811 @default.
• W2509155656 hasRelatedWork W2584477428 @default.
• W2509155656 hasRelatedWork W2618633120 @default.
• W2509155656 hasRelatedWork W2743303184 @default.
• W2509155656 hasRelatedWork W2749854074 @default.
• W2509155656 hasRelatedWork W2790373036 @default.
• W2509155656 hasRelatedWork W2791994046 @default.
• W2509155656 hasRelatedWork W2896992392 @default.
• W2509155656 hasRelatedWork W2913166062 @default.
• W2509155656 hasRelatedWork W2997346969 @default.
• W2509155656 hasRelatedWork W3024792029 @default.
• W2509155656 hasRelatedWork W3095897970 @default.
• W2509155656 isParatext "false" @default.
• W2509155656 isRetracted "false" @default.
• W2509155656 magId "2509155656" @default.
• W2509155656 workType "article" @default.