Evaluation of ALADIN NWP model forecasts by IR10.8 µm and WV06.2 µm brightness temperatures measured by the geostationary satellite Meteosat Second Generation
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60460709%3A41330%2F22%3A91726" target="_blank" >RIV/60460709:41330/22:91726 - isvavai.cz</a>
Výsledek na webu
<a href="https://www.sciencedirect.com/science/article/pii/S0169809521004762?via%3Dihub" target="_blank" >https://www.sciencedirect.com/science/article/pii/S0169809521004762?via%3Dihub</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.atmosres.2021.105920" target="_blank" >10.1016/j.atmosres.2021.105920</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Evaluation of ALADIN NWP model forecasts by IR10.8 µm and WV06.2 µm brightness temperatures measured by the geostationary satellite Meteosat Second Generation
Popis výsledku v původním jazyce
An evaluation of forecasts by ALADIN numerical weather prediction model is performed by comparing synthetic and measured IR10,8 mu m (Infrared channel with a wavelength of 10,8 mu m) and WV06,2 mu m (Water vapour channel with a wavelength of 6,2 mu m) brightness temperatures (BTs) by the geostationary satellite Meteosat Second Generation. To calculate synthetic satellite images, we used a radiative transfer model RTTOV v11,3, as implemented in the ALADIN model. The evaluation of the forecasts is performed for summer month June 2020 and winter month February 2021 and for lead times from 1 to 72 h. The model horizontal resolution is 2,3 km and the verification domain covers a large part of Europe. As for verification parameters, we calculated bias, root-mean-square error, correlation coefficient (PC), Fraction Skill Score and a technique that take into account the relative position of the verified objects. We diagnosed relationships, measured by PC, between the forecasted and measured BTs on one side a
Název v anglickém jazyce
Evaluation of ALADIN NWP model forecasts by IR10.8 µm and WV06.2 µm brightness temperatures measured by the geostationary satellite Meteosat Second Generation
Popis výsledku anglicky
An evaluation of forecasts by ALADIN numerical weather prediction model is performed by comparing synthetic and measured IR10,8 mu m (Infrared channel with a wavelength of 10,8 mu m) and WV06,2 mu m (Water vapour channel with a wavelength of 6,2 mu m) brightness temperatures (BTs) by the geostationary satellite Meteosat Second Generation. To calculate synthetic satellite images, we used a radiative transfer model RTTOV v11,3, as implemented in the ALADIN model. The evaluation of the forecasts is performed for summer month June 2020 and winter month February 2021 and for lead times from 1 to 72 h. The model horizontal resolution is 2,3 km and the verification domain covers a large part of Europe. As for verification parameters, we calculated bias, root-mean-square error, correlation coefficient (PC), Fraction Skill Score and a technique that take into account the relative position of the verified objects. We diagnosed relationships, measured by PC, between the forecasted and measured BTs on one side a
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10509 - Meteorology and atmospheric sciences
Návaznosti výsledku
Projekt
—
Návaznosti
S - Specificky vyzkum na vysokych skolach
Ostatní
Rok uplatnění
2022
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
ATMOSPHERIC RESEARCH
ISSN
0169-8095
e-ISSN
1873-2895
Svazek periodika
2022
Číslo periodika v rámci svazku
265
Stát vydavatele periodika
CZ - Česká republika
Počet stran výsledku
20
Strana od-do
1-20
Kód UT WoS článku
000790517900003
EID výsledku v databázi Scopus
2-s2.0-85119490216