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<supportEmail caption="Support">icrc2007@icrc2007.unam.mx</supportEmail>
<title>30th International Cosmic Ray Conference</title>
<description>The 30th International Cosmic Ray Conference will be held from July 3, 2007 to July 11, 2007 in Merida, Yucatan, Mexico.</description>
<participants></participants>
<closed>True</closed>
<location>
 <name>Merida, Mexico</name>
 <address></address>
 <room></room>
</location>
<startDate>2007-07-03T08:00:00</startDate>
<endDate>2007-07-11T19:00:00</endDate>
<creationDate>2005-09-26T05:04:53</creationDate>
<modificationDate>2024-04-12T17:46:55</modificationDate>
<timezone>Mexico/General</timezone>
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  <title>Dr.</title>
  <name first="José" middle="" last="Valdés"></name>
  <organization>IGeof-UNAM</organization>
  <emailHash>40af9343b8bb9d18708b4f0252d5f53c</emailHash>
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 <track>SH.3.6</track>
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  <name>Poster</name>
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 <title>Interconnections Between Forbush Cosmic Ray Decreases and Atlantic Hurricanes Development.</title>
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   <title>Prof.</title>
   <name first="Stilian" middle="" last="Kavlakov"></name>
   <organization>Bulgarian Academy of Sciences</organization>
   <emailHash>e78c100a2eb56c41b9667f93ed6c7149</emailHash>
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   <title>Prof.</title>
   <name first="Stilian" middle="" last="Kavlakov"></name>
   <organization>Bulgarian Academy of Sciences</organization>
   <emailHash>e78c100a2eb56c41b9667f93ed6c7149</emailHash>
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   <title>Prof.</title>
   <name first="James" middle="" last="Elsner"></name>
   <organization>Florida State University</organization>
   <emailHash>8f8a3a08ff2cdb276785d6a92a554f23</emailHash>
  </user>
  <user>
   <title>Prof.</title>
   <name first="Jorge" middle="" last="Perez-Peraza"></name>
   <organization>Instituto de Geofisica, UNAM, C.U., Coyoacan, 04510, Mexico, D.F. Mexico.</organization>
   <emailHash>a41e3fcdbf4ce4c3e372987593912516</emailHash>
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 <location>
  <name>Merida, Mexico</name>
  <address></address>
  <room>Regency (Hyatt)</room>
 </location>
 <startDate>2007-07-06T14:45:00</startDate>
 <endDate>2007-07-06T14:45:00</endDate>
 <abstract>The Forbush decreases, recorded during 1951-2005 neutron measurements on Climax
Cosmic Ray Station were used, estimating their number per year F(n)  and calculating
their total yearly decrease F(t). They were investigated together with certain
parameters of the hurricanes recorded over a large Atlantic Ocean area, situated
between 25 and 60 degrees West, and 8 and 23 degrees North. In that area the water
surface temperature is practically constant and the possibility of hurricane
formation is equally distributed over it. The hourly data for hurricane maximum
rotational wind velocity (W) was used to calculate: the kinetic energy as W2 and the
total yearly accumulated hurricane increase of this velocity as dW/dt.
It was found that both these parameters correlated well with F(n) and F(t). That
indicates the existence of some parallel or even interconnected high atmosphere
processes triggering the hurricane formation. From the other side that extend the
possibilities for earlier hurricane forecasts.</abstract>
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