An analysis of simulated and observed storm
characteristics
- Can we expect a change in the future?
R.E. Benestad, CES, June 01 2010
Number of cyclones:
RCM
analysis
CCI
(Benestad & Chen, 2006) righttoleftmark
No change in storm frequency?
RCM:
N corresponds
|v| too high
...or simulated wind speeds?
•CCI
•triangulation
Method: storm characteristics
RCM: storms too small
too strong.
Gradient
/media/ces/Benestad_Rasmus_CES_2010.pdf
We are hoping to find time to improve this glossary. Only a few items are available. For your relevant search, please click on one of the letters below:
A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö
A
A: Icelandic abbreviation of East (compass direction, easterly, eastern).
ANA: Icelandic abbreviation of Eastnorthesast (compass direction).
ASA: Icelandic
/weather/articles/nr/1208
We are hoping to find time to improve this glossary. Only a few items are available. For your relevant search, please click on one of the letters below:
A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö
A
A: Icelandic abbreviation of East (compass direction, easterly, eastern).
ANA: Icelandic abbreviation of Eastnorthesast (compass direction).
ASA: Icelandic
/weather/articles/nr/1208/