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Sökning: onr:"swepub:oai:DiVA.org:uu-418900" > Statistics of sea-e...

Statistics of sea-effect snowfall along the Finnish coastline based on regional climate model data

Olsson, Taru (författare)
Finnish Meteorol Inst, PL 503, Helsinki 00101, Finland.
Luomaranta, Anna (författare)
Finnish Meteorol Inst, PL 503, Helsinki 00101, Finland.
Jylha, Kirsti (författare)
Finnish Meteorol Inst, PL 503, Helsinki 00101, Finland.
visa fler...
Jeworrek, Julia (författare)
Univ British Columbia, Dept Earth Ocean & Atmospher Sci, Vancouver, BC, Canada.
Perttula, Tuuli (författare)
Finnish Meteorol Inst, PL 503, Helsinki 00101, Finland.
Dieterich, Christian (författare)
Swedish Meteorol & Hydrol Inst, Norrkoping, Sweden.
Wu, Lichuan (författare)
Uppsala universitet,Luft-, vatten- och landskapslära
Rutgersson, Anna, 1971- (författare)
Uppsala universitet,Luft-, vatten- och landskapslära,Uppsala Univ, Ctr Nat Hazards & Disaster Sci CNDS, Uppsala, Sweden.
Makela, Antti (författare)
Finnish Meteorol Inst, PL 503, Helsinki 00101, Finland.
visa färre...
Finnish Meteorol Inst, PL 503, Helsinki 00101, Finland Univ British Columbia, Dept Earth Ocean & Atmospher Sci, Vancouver, BC, Canada. (creator_code:org_t)
2020-06-18
2020
Engelska.
Ingår i: Advances in Science and Research. - : COPERNICUS GESELLSCHAFT MBH. - 1992-0628 .- 1992-0636. ; 17, s. 87-104
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
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  • The formation of convective sea-effect snowfall (i.e., snow bands) is triggered by cold air outbreaks over a relatively warm and open sea. Snow bands can produce intense snowfall which can last for several days over the sea and potentially move towards the coast depending on wind direction. We defined the meteorological conditions which statistically favor the formation of snow bands over the north-eastern Baltic Sea of the Finnish coastline and investigated the spatio-temporal characteristics of these snow bands. A set of criteria, which have been previously shown to be able to detect the days favoring sea-effect snowfall for Swedish coastal area, were refined for Finland based on four case study simulations, utilizing a convection-permitting numerical weather prediction (NWP) model (HARMONIE-AROME). The main modification of the detection criteria concerned the threshold for 10 m wind speed: the generally assumed threshold value of 10 ms 1 was decreased to 7 ms(-1). The refined criteria were then applied to regional climate model (RCA4) data, for an 11-year time period (2000-2010). When only considering cases in Finland with onshore wind direction, we found on average 3 d yr(-1) with favorable conditions for coastal sea-effect snowfall. The heaviest convective snowfall events were detected most frequently over the southern coastline. Statistics of the favorable days indicated that the lower 10 m wind speed threshold improved the representation of the frequency of snow bands. For most of the favorable snow band days, the location and order of magnitude of precipitation were closely captured, when compared to gridded observational data for land areas and weather radar reflectivity images. Lightning were observed during one third of the favorable days over the Baltic Sea area.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Meteorologi och atmosfärforskning (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Meteorology and Atmospheric Sciences (hsv//eng)

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