[seminar] SEMINAR na IF-u u CETVRTAK, 27. 05. 2010.

[Berislav Horvatić]

ZAJEDNIČKI KOLOKVIJ

FIZIČKOG ODSJEKA PMF-a I INSTITUTA ZA FIZIKU

      Institut za fiziku, Bijenička cesta 46,

      predavaonica u zgradi Mladen Paić

      četvrtak, 27. svibnja 2010, u 15:00 sati

       
     
      The mechanism of severe bora wind

       
     
      Prof. dr. sc. Branko Grisogono
     
       

      Geofizički odsjek Prirodoslovno-matematičkog fakulteta

      Sveučilišta u Zagrebu, Horvatovac 95, HR-10000 Zagreb

       

      E-mail: bgrisog at gfz.hr

       
     
      A gusty downslope windstorm which blows at the eastern Adriatic coast is called bora. There has been substantial progress in bora observations and measurements, understanding, modeling and its more detailed prediction during the last 25 years. It was generally thought before that bora was a falling, mostly thermodynamically driven wind; however, (severe) bora is primarily governed by mountain wave breaking. Understandings of bora interactions and influences on other processes have taken place as well, most notably in the air-sea interaction, but are not completed yet. The focus here is on stronger bora flows at the NE Adriatic coast.

      http://www.gfz.hr/osobne_stranice/grisogono/branko_home.htm

       
     
      voditelji seminara   H. Buljan (FO)   &   B. Horvatić  i  M. Kralj (IF)
     
-------------- next part --------------
An HTML attachment was scrubbed...
URL: <http://www.phy.hr/pipermail/seminar/attachments/20100517/dac72f63/attachment.htm>
-------------- next part --------------
A non-text attachment was scrubbed...
Name: not available
Type: image/jpeg
Size: 5394 bytes
Desc: not available
URL: <http://www.phy.hr/pipermail/seminar/attachments/20100517/dac72f63/attachment.jpeg>