NO +60:23:18 +11:33:37 147 P
184 HALDEN NO +59:07:21 +11:23:18 8 P
185 SUOLOVUOPMI NO +69:35:17 +23:31:54 377 P
188 GLOMFJORD NO +66:49:00 +13:58:59 39 T
190 KARASJOK NO +69:28:00 +25:30:11 129 TP
191 KJOEREMSGRENDE NO +62:06:00 +09:03:00 626 T
21
192
/media/ces/CES_D2.4_task1.pdf
landshlutum.
Auk þess er meðalhiti síðustu tíu ára örlítið hærri en meðalhiti
tíu áranna á undan.
hiti °C vik vik
Stöð 2009–2018 1961–1990 1999–2008
Reykjavík 5,4 1,0 0,2
Stykkishólmur 4,8 1,3 0,3
Akureyri 4,4 1,2 0,1
Dalatangi 4,8 1,3 0,3
Meðalhiti og vik síðustu tíu ára í Reykjavík, Stykkishólmi, á Akureyri
og Dalatanga.
Meðalhiti einstakra ára er í öllum tilfellum vel yfir meðaltali
/media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf
need inclusion (van der Keur et al. 2008). The complete suite of uncertainties
has been referred to as the uncertainty cascade (Hulme and Carter 1999; Katz 2002;
Foley 2010).
Making climate change adaptation decisions is particularly difficult since they rely
on uncertainties related to climate projections as well as to developments in natural
systems and sectors that are affected by other
/media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf
The full list
of examples in order of their appearance in Tables 2 and 3 are:
(1) Grampian (Polhill et al., 2010);
(2) Hase I (Newig et al., 2008);
(3) Wadden Sea (Engelen, 2004);
(4) Zürich (Pahl-Wostl and Hare, 2004);
(5) Nîmes (Etienne et al., 2008b);
(6) Hase II (Newig et al., 2008);
(7) Iskar (Phase I) (Daniell, 2008);
(8) Moorlands (Hare, 1999);
(9) Ebro (Valkering et al., 2009);
1A
/media/loftslag/Hare-2011-ParticipatoryModelling.pdf
methodology is widely utilized by many automatic earthquake detectors, but instead of having
window lengths on the order of minutes, like the ALERT module, they have window durations
on the order of seconds. A longer STA window duration will make the module less sensitive to
small signals (Trnkoczy, 1999). Additionally, the total duration of the STA and LTA windows
may not exceed 24 hours
/media/vedurstofan-utgafa-2021/VI_2021_008.pdf
; Jylhä et al., 2008; Räisänen, 2008) and to de-
crease snowmelt floods, which are currently the largest floods in
most parts of Finland. Significant changes in seasonality of runoff
and floods may occur in areas where a large proportion of runoff
is from snowmelt (e.g. Lettenmaier et al., 1999; Bates et al., 2008).
Finland extends from 70 North with sub-arctic climate to 60
North in the margins
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
sheet: Greenland
Climate Network 1995–1999, Journal of Geophysical Research, 106(D24), 33,951–33,964.
Stendel, M., J. H. Christensen, G. Aðalgeirsdóttir, N. Kliem, and M. Drews (2007), Regional
climate change for Greenland and surrounding seas part I: Atmosphere and land surface, in
Danish Climate Centre Report, vol. 07-02, Danish Meteorological Institute.
Thomsen, H., L.Thorning, and O. Olesen (1989
/media/ces/ces_geus_paakitsoq_full_report.pdf
with Beaufort number 2 is expected
to increase the most in the future and strong winds (Beaufort 4 to 10) to decrease.
Wind direction
Wind directions in Iceland tend to be controlled by orography but, as CORDEX data from
the reference period reveals, SW-NE components are the most common in many areas. The
NE winds are often cool and associated with cold weather (Olafsson, 1999). When winds
/media/vedurstofan-utgafa-2017/VI_2017_009.pdf