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21 Monthly mean 10-m wind speed for different wind directions over Þórisvatn ...... 30
6
1 Introduction
In the spring of 2013, the Icelandic Meteorological Office (IMO) started a reanalysis project,
using the HARMONIE numerical weather prediction model. Operationally, this model has been
in use at IMO since the autumn of 2011, and has proven
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
with 20% and 2% for the HIRHAM experiments
using HadAM3H and with 30% and 7% for the ECHAM-
driven experiments for Middle Europe and Scandinavia,
respectively.
[18] RCM output is not available for the entire period
1961–2100 because transient RCM simulations are com-
putationally very demanding. Instead two 30-year time
slices are available; one representative for the climate in
the period 1961–1990
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
; fax: +358 20 490 2590.
E-mail address: Noora.Veijalainen@ymparisto.fi (N. Veijalainen).
Journal of Hydrology 391 (2010) 333–350
Contents lists available at ScienceDirect
Journal of Hydrology
journal homepage: www.elsevier .com/ locate / jhydrol
Author's personal copy
narios from GCMs or RCMs, and with different emission scenarios
(e.g. Menzel et al., 2006; Minville et al., 2008; Prudhomme and Da
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
GCM simulations of mean annual
surface air temperature: mean fields in degrees centigrade during the 1961–90
control period, differences in degrees between the control period and the 2021–
50 reference period, and linear trends in degrees per decade within the 2004–50
period, for the SMHI-RCAO, the MetNo-HIRHAM, and the DMI-HIRHAM5. . . . 30
9 Mean annual total precipitation in millimetres per
/media/ces/2010_005_.pdf
measurements are still performed
with newer instruments today, making it the worlds longest sea level data series (SMHI, 2018b).
Today, The Swedish Meteorological and Hydrological Institude (SMHI) runs a network of 24 tide
gauges that measure sea level averaged over 10 minute periods in a relative elevation system. The
data is gathered every hour and presented online2 within 30 minutes, relative
/media/vedurstofan-utgafa-2020/VI_2020_005.pdf
the principalmethods have not changed much over the years, theamount of field work has varied. In the first 15 yearsthe monitoring programme at Storbreen was com-prehensive, often three or more snow density pits
were dug, snow depth was measured at about 600points and ablation was measured on 30 stakes
evenly distri uted on the glacier (Liestøl 1967).Based on experience of the snow pattern, the ob-
servations
/media/ces/GA_2009_91A_4_Andreassen.pdf
of the glacier is projected to be reduced by 30 %
with respect to the present at the end of this century. If the
climate warms, as suggested by most of the climate change
scenarios, the model projects this glacier to almost disappear
by the end of the 21st century. Runoff from the glacier is
predicted to increase for the next 30–40 yr and decrease after
that as a consequence of the diminishing ice-covered area
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
H. Haraldsson and Tómas Jóhannesson .............................................................................. 29
The mass balance of Brúarjökull, outlet of N-Vatnajökull Ice cap Iceland, in the 20th and 21st
century
Chris Polashenski ................................................................................................................... 30
Applications of terrestrial lidar
/media/vatnafar/joklar/Reykholt-abstracts.pdf