37 results were found for JZMOR e la prevenzione della frode: sicurezza a portata di mano.

Results:

• 21. Paper-Olafur-Rognvaldsson_92

  ) and Jónsdóttir (2008). Therefore, comparison of measured and simulated water balance cannot be di- rectly used for validation of the model-generated precipitation. According to the non-scaled MM5 output for the period 1961–1990, mean precipitation for the whole of Iceland was 1790 mm y−1. After scaling the precipitation, this value was reduced to 1750mm y−1, i.e. by approximately 2%. This difference /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 22. VI_2015_005

  Franz Josef Land. The western boundary at 71 W excludes Hudson Bay and Foxe Basin, both associated with their own storm climate. Baffin Bay is included in its entirety, since storm activity in that region is closely linked to that over the western North Atlantic (Dacre & Gray, 2009). The eastern boundary at 55 E is chosen to completely include the Barents Sea. This results in an area of 21,625,566 /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 23. 2013_001_Nawri_et_al

  is then proportional to the mean cube of wind speed, E = 1 2 r¯ A3G(1+3=k) ; (3) where r¯ is average air density. Wind power density only depends on atmospheric variables, and is therefore most appropriate for turbine-independent evaluations of wind energy potential, such as for wind atlases. To be able to determine the actual power or energy, which can be extracted from the atmosphere, specific information /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 24. 2010_003rs

  ca ti o n s fo r th e la rg est e a rt h q u a ke s w it h in t h e S IS Z b et w ee n 1 7 0 6 a n d 2 0 0 8 d en o te d b y w h ite fil le d c ir cles. E stim a te d f a u lt p la n es o f h is to ric a l ea rt h q u a ke s a re s h o w n a s w h ite , th ick li n es ( fr o m R o th , 2 0 0 4 ). F a u lt p la n es f ro m 1 9 9 8 ( V o g fj ö rd et a l. , 2 /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 25. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  Reykjavı´k IS-101, Iceland 2 Centre National de la Recherche Scientifique, Universite´ de Toulouse, Laboratoire d’Etudes en Ge´ophysique et Oce´anographie Spatiale, Universite´ de Toulouse, 14 Avenue Edouard Belin, Toulouse FR-31400, France 3 National Space Institute, Technical University of Denmark, Lyngby DK-2800, Denmark Keywords Remote sensing; glacier mass balance; regional warming /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 26. VI_2014_001

  at each site i with the same method used to estimate qR(D;T ), but instead of pooling AMF series for a given duration D from different sites, the estimation is made individually for each site i by pooling AMF series for different durations D (see Crochet, 2012c). The index flood µi(D), is modeled at each site i as a continuous function of D, as follows: µi(D) = µi 1+(D=Di)li ; (5) where µi, Di /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 27. VI_2015_007

  with the same method used to estimate qR(D;T ), but instead of pooling AMF series for a given duration D from different sites, the estimation is made individually for each site i by pooling AMF series for different durations D. The index flood, µi(D), is modelled at each site i as a continuous function of D, as follows: 12 µi(D) = µi 1+(D=Di)li ; (6) where µi, Di and li are basin dependent parameters /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

• 28. Guidelines2-for-rapporteurs

  ). This can be helpful with respect to finding a common structure in presenting as well in session reporting (for which angles mentioned in the opening session statements of the Workshop participants can provide checkpoints).” Session rapporteur allocation M o n d a y 2 9 . 8 Y u a n g Z h e n g A t h a n a s i o s V o t s i s E i v i n d J u n k e r M i c h a e l L a i h o H e c to r /media/loftslag/Guidelines2-for-rapporteurs.pdf

• 29. Reykholt-abstracts

  Berthier3 1Institute of Earth Sciences, University of Iceland 2The Icelandic Meteorological Office 3Centre National de la Recherche Scientifique, Laboratoire d’Etudes en Géophysique et Océanographie Spatiale, Université de Toulouse, France * Corresponding author, e-mail: sg (at) hi.is ABSTRACT We assess the mass balance changes of the ~81 km2 Eyjafjallajökull ice cap in South Iceland, over three /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 30. VI_Arsskyrsla_2018_vef

  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 3 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