81 results were found for V Ισπανική ανάλυση【WWW,RT33,TOP】코드b77】ινδικό τοτόുβάζω κάρβουναޗδιόστοτοᇌζωντανά στοιχήματα σε πραγματικό χρόνοླྀΤζίνρο Τοτόຮποδόσφαιρο της μιανμάρ∼Εθνική ομάδα της Σαουδικής Αραβίας☁ποδόσφαιρο του Σαν Μαρίνοჭ.byq/.
/EPP 2
Stakeholders analysis
26 August 2011 PM/YZ/EPP 3
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/media/loftslag/Group5-Stakeholders_involvement.pdf
in the period 6th to the 22nd, eight from ships and one from land. The icebergs were closest to land at 66°28,81'N og 21°23,86'V and close to Selsker (66°07,5N og 21°31'V).
No seaice was in the Greenland Strait in August and northeasterly winds prevailed in the area
/sea-ice/monthly/2009/nr/2330
2008)
together with a regression line through this data set and a regression line derived for a data set
of more than a hundred valley glaciers (Bahr and others, 1997). The regression lines are of the
form
v = csg ; (5)
where v and s are glacier volume and area, respectively. The coefficient and exponent for the
Icelandic ice caps are c = 0:048, g = 1:23, when the area and volume are expressed
/media/ces/ces-glacier-scaling-memo2009-01.pdf
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
In Chapter 3 we focus on the following monthly averages: Near-surface 2 meter temperature
(TAS), total precipitation (TP), and sea ice cover (SI). In Chapter 4 we add surface air
pressure (PSL) and snow cover thickness (SNCT). The following daily fields will be studied
as well: Near-surface wind speeds, (U and V sfcWind), maximum near-surface 2 meter
temperature (TASMAX), minimum mean-surface 2 meter
/media/vedurstofan-utgafa-2017/VI_2017_009.pdf
TíðaskarðFaxaflsjObs.ForecastMeteogramInfo.Obs. data
Tjörnes - GerðibrekkaNorth EsjObs.ForecastMeteogramInfo.Obs. data
TorfurNorth EsjObs.Info.Obs. data
Return to the top of the page
U
UpptyppingarCentralsjObs.Info.Obs. data
Return to the top of the page
V
VaðlaheiðiNorth EsjObs.Info.Obs. data
Vaðlaheiði IINorth EsjObs.Info.Obs. data
VatnaleiðFaxaflsjObs.ForecastMeteogramInfo.Obs. data
/weather/stations/
all sites was calculated (RMSET ):
RMSET (%) =
1
N
N
i=1
v
u
u
t1
L
L
l=1
Qi(D;Tl) bQi(D;Tl)
Qi(D;Tl)
2
x100 (7)
where Qi(D;Tl) is the reference flood quantile at gauged site i and return period Tl , calculated
with the GEV distribution fitted to the observed AMF series and bQi(D;Tl) is the estimated flood
quantile, calculated with the IFM ( bQi(D;T ) = bµi(D)qR(D;T )). RMSET was ranked
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf