SwePub
Sök i LIBRIS databas

  Utökad sökning

WFRF:(Svensson Filip)
 

Sökning: WFRF:(Svensson Filip) > Impact of flow-depe...

Impact of flow-dependent horizontal diffusion on resolved convectionin AROME.

Bengtsson, Lisa, 1981- (författare)
Sveriges meteorologiska och hydrologiska institut (SMHI), Norrköping
Tijm, Sander (författare)
Vána, Filip (författare)
visa fler...
Svensson, Gunilla (författare)
Stockholms universitet,Meteorologiska institutionen (MISU)
visa färre...
 (creator_code:org_t)
2012
2012
Engelska.
Ingår i: Journal of Applied Meteorology and Climatology. - 1558-8424 .- 1558-8432. ; 51:1, s. 54-67
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • Horizontal diffusion in numerical weather prediction models is, in general, applied to reduce numerical noise at the smallest atmospheric scales. In convection-permittingmodels, with horizontal grid spacing on the order of 1–3 km, horizontal diffusion can improve themodel skill of physical parameters such as convective precipitation. For instance, studies using the convection-permitting Applications of Research to Operations at Mesoscale model (AROME) have shown an improvement in forecasts of large precipitation amounts when horizontal diffusion is applied to falling hydrometeors. The nonphysical nature of such a procedure is undesirable, however. Within the current AROME, horizontal diffusion is imposed using linear spectral horizontal diffusion on dynamicalmodel fields. This spectral diffusion is complemented by nonlinear, flow-dependent, horizontal diffusion applied on turbulent kinetic energy, cloud water, cloud ice, rain, snow, and graupel. In this study, nonlinear flowdependent diffusion is applied to the dynamical model fields rather than diffusing the already predicted falling hydrometeors. In particular, the characteristics of deep convection are investigated. Results indicate that, for the same amount of diffusive damping, the maximum convective updrafts remain strong for both the current and proposed methods of horizontal diffusion. Diffusing the falling hydrometeors is necessary to see a reduction in rain intensity, but amore physically justified solution can be obtained by increasing the amount of damping on the smallest atmospheric scales using the nonlinear, flow-dependent, diffusion scheme. In doing so, a reduction in vertical velocity was found, resulting in a reduction in maximum rain intensity.

Ämnesord

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

Nyckelord

atmosfärvetenskap och oceanografi
Atmospheric Sciences and Oceanography

Publikations- och innehållstyp

ref (ämneskategori)
art (ämneskategori)

Hitta via bibliotek

Till lärosätets databas

Sök utanför SwePub

Kungliga biblioteket hanterar dina personuppgifter i enlighet med EU:s dataskyddsförordning (2018), GDPR. Läs mer om hur det funkar här.
Så här hanterar KB dina uppgifter vid användning av denna tjänst.

 
pil uppåt Stäng

Kopiera och spara länken för att återkomma till aktuell vy