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/.
• Analyse future snow scenarios
Introduction Data & Methods Results
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/media/ces/Dyrrdal_Anita_CES_2010.pdf
2015, 2025, 2035 and 2050
North (Blanda) East (Karahnjukar) South (Thorisvatn)
Change in average inflow to the main storage reservoirs
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Temperature corrected
Transformation of climate measurements
•Change in temperature
• 0.75 °C/100y 1950-1975
• 1.55
/media/ces/Linnet_Ulfar_CES_2010.pdf
vuosille 2010–2040; Trafi 3/2010
Shares of elderly drivers without accidents and/or fines (in the previous year)
by age category, and comparison with very young drivers
Source: Mikkonen, V. (2010), Seniorikuljettajien seurantaindeksi, Trafi 5/2010
Aggregate risk of motor vehicle collision (per million vehicle km) in Finland (“dry”
road vs. icy/snowy road surface) (2003-2006).
(a) Based
/media/loftslag/Case_B___Road_transport_operation_and_infrastructure_planning.pdf
-CALPUFF model is not using plume height estimates
as an input parameter. The model itself solves the equations describing the rising of the mixture
in the atmosphere and calculates the top-plume height by using some physical parameters as
the vertical mixture velocity (V) and the radius of the vent (R). Based on these two parameters,
V and R, we get an estimate of the mass flow rate and we
/media/vedurstofan-utgafa-2020/VI_2020_004.pdf
water.
Since, in this study, the focus is on large-scale storm systems, persisting for at least one day,
variability on shorter time-scales (mainly the diurnal cycle and atmospheric tides) is eliminated
by calculating averages from the four 6-hourly reanalysis fields of each day (6-hourly precip-
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Figure 1. Top: Average fields of 500 hPa geopotential height in winter (DJF 1989-90)
and summer (JJA
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf
for the cases where abstractions and
irrigation are not included (Table 3, top) and included
(Table 3, bottom). The results are spatially averaged, mean
annual values for the 15-year period. The net recharge is
defined as the outflow from the root zone minus the sum of
evapotranspiration and net flow from the groundwater zone
to the overland compartment for the grids where the soil
profile
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
-m temperature is increased by the external surface scheme, the magnitude of temporal
variability, related to changes in the near-surface radiation balance, is improved.
17
Figure 8. Monthly averages of simulated 2-m air temperature from either SURFEX or
projected from the two lowest HARMONIE model levels, in comparison with station mea-
surements. In the top panels, all hourly values are used
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
Forsíðumynd: Svava Björk Þorláksdóttir mælir með öldustilli
niður á festur í Iðu í Hvítá. Ljósmynd: Njáll Fannar Reynisson.
V E Ð U R S T O F A Í S L A N D S / Á R S S K Ý R S L A 2 0 1 8
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Viðburðaríkt ár er að baki
hjá starfsfólki Veðurstofunnar
enda felast jafnan margar og
fjöl breyttar áskoranir í vöktun
og rannsóknum á náttúru -
öflum landsins.
Loftslagsmál eru mjög á
döfinni enda stærsta
/media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf
), Torfajökull (To) and Mýrdalsjökull (M) ice caps.
V: automatic weather station at Vík in Mýrdalur. On the inset map of Iceland: location
of the study area as well as Langjökull (L), Hofsjökull (H) and Vatnajökull (Va) ice
caps. The plot shows the elevation distribution of the E, Ti and To ice caps as area
(km2) per 10 m elevation interval.
Digital Elevation models calculated using:
a) SPOT 5 HRS
/media/ces/glacier_mass_balance_poster.pdf