Pregled bibliografske jedinice broj: 570492
Comparison and validation of satellite-based overshooting top detection methods
Comparison and validation of satellite-based overshooting top detection methods // Proceedings - 6th European Conference on Severe Storms (ECSS 2011), Palma de Mallorca, Spain, 03-07 October 2011
Palma de Mallorca, Španjolska, 2011. (poster, međunarodna recenzija, cjeloviti rad (in extenso), znanstveni)
CROSBI ID: 570492 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Comparison and validation of satellite-based overshooting top detection methods
Autori
Mikuš, Petra ; Bedka, Kristopher ; Strelec Mahović, Nataša
Vrsta, podvrsta i kategorija rada
Radovi u zbornicima skupova, cjeloviti rad (in extenso), znanstveni
Izvornik
Proceedings - 6th European Conference on Severe Storms (ECSS 2011), Palma de Mallorca, Spain, 03-07 October 2011
/ - , 2011
Skup
6th European Conference on Severe Storms (ECSS 2011)
Mjesto i datum
Palma de Mallorca, Španjolska, 03.10.2011. - 07.10.2011
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
overshooting tops; satellite-based detection methods
Sažetak
Overshooting convective cloud tops (OT), dome-like protrusions above a cumulonimbus anvil, indicate the location of vigorous updrafts where severe weather including heavy rainfall, hail, strong winds and tornadoes most often occurs. OTs are apparent in satellite data with a lumpy textured appearance in visible channel imagery. Since visible channel imagery is only available during daytime, meteorologists must also use the infrared (IR) channels for observing and objective detection of OTs. The aim of this investigation is to compare the detection characteristics and relative accuracy of several different satellite–based OT detection methods. Research by the authors has shown that OTs can be detected from the satellite data using the brightness temperature difference (BTD) of the water vapor and the IR channel (6.2–10.8 μm), BTD of the ozone and IR channel (9.7–10.8 μm) or BTD of carbon dioxide and IR channel (13.4–10.8 μm). A combination of the 6.2-10.8 μm and 9.7-10.8 μm BTDs can also be used. All these methods include thresholds for both IR brightness temperature and the BTD. A more complex method, called IRW-texture, includes a combination of infrared channel brightness temperature and spatial gradient criteria with a numerical weather prediction model tropopause temperature forecast to detect OT signatures at their characteristic spatial scale. The theoretical background of all mentioned methods will be explained and the results of detection will be compared with the High Resolution Visible (HRV) satellite images during day-time in order to validate each method.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Projekti:
004-1193086-3036 - Oluje i prirodne katastrofe u Hrvatskoj (Ivančan-Picek, Branka, MZOS ) ( CroRIS)
Ustanove:
Državni hidrometeorološki zavod