the land are identical. As
discussed previously, the DMI-HIRHAM5 results are suspect with regard to spatial variability of
SAT trends. However, from the other two RCM simulations, relative enhancement of warming
between the surrounding sea area and the Icelandic highlands can be determined. It is found that,
according to the SMHI-RCAO, this enhancement is 24%, and 46% for the MetNo-HIRHAM
/media/ces/2010_005_.pdf
with l l2, containing the region with frequent cyclone
activity to the northeast of Iceland. Then, of the total study area, 22% fall into the western sector
(itself broken up into 70% ocean and 30% land), 32% in the central sector (77% ocean, 23%
land), and 46% in the eastern sector (44% ocean, 56% land).
The average seasonal cyclone occurrences over the ocean and land areas in different sectors
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf