79 results were found for [77AGG. COM]m88 slot v slot remi slot lpo88 slot g200 slot slot qris fo9.

Results:

• 31. hafisskyrsla-23-mars-2011

  °35V 5. 66°31N 024°55V 6. 66°42N 024°26V 7. 67°03N 023°44V 8. 67°14N 023°29V 9. 67°33N 022°26V Var ísinn 7-9/10 að þéttleika og sást greinileg nýmyndun inn á milli þar sem hann var gisnari. Ekki var að sjá stóra jaka eða borgarísjaka í jaðri ísins svo gera má ráð fyrir að hann sjáist ekki vel á ratsjá. Út frá ísröndinni sáust nokkrar ísdreifar og voru teknir staðir á þeim. 1. 65°51N 026°39V /media/hafis/skyrslur_lhg/hafisskyrsla-23-mars-2011.pdf

• 32. isskyrsla_14122010

  segir hann að þetta er dreifar og þéttur ís hjá honum, lofthiti -5°c. Staður á LLDM er N67.12,10, W020.04,44. LLDM er á leið til Ísafjarðar til að landa rækju þar. Eftir lendingu í Reykjavík upplýsti TFB að LLDM hefði haft samband vegna hafíss. Hafði kl.0030 siglt framá 30-30 metra háan borgarís á stað: 67°10,45´n-020°14,7´v. Sást allvel í ratsjá. Þéttleiki hafíss í næsta nágrenni um 3/10 /media/hafis/skyrslur_lhg/isskyrsla_14122010.pdf

• 33. norsem_lund

  more events in the vicinity in the next two months. These aftershocks are interesting as aftershocks to M4+ events are not always observed in Sweden and Finland. The Bothnian Bay is one of the most seismically active areas in continental Fennoscandia, but the cause of the seismicity is still not well known. Until recently, the offshore areas have been poorly monitored by the national seismic /media/norsem/norsem_lund.pdf

• 34. ces-glacier-scaling-memo2009-01

  difference between the band and the maximum altitude of the glaciers ymax Dgi = ri gi ; ri = DSa2 (ymax yi) nj=1(ymax y j)g j : (12) The second step is carried out after the lowest glaciated elevation bands have been altered by the reduction in the glaciated area at the lowest altitudes. This procedure to distribute the reduction in glaciated area with altitude is clearly quite crude /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 35. Tornado_Impacts_-_FMI_Presentation

  The Economic and Societal Impacts of Tornadoes Kevin M. Simmons Austin College Fulbright Research Scholar International Centre for GeoHazards Oslo, Norway Economic and Societal Impacts of Tornadoes By Kevin M. Simmons and Daniel Sutter © 2010, 296 pages in paperback ISBN: 978-1-878220-99-8 AVAILABLE NOVEMBER 2010 from the American Meteorological Society and the University of Chicago Press /media/loftslag/Tornado_Impacts_-_FMI_Presentation.pdf

• 36. Dataseries and components

  Analysed components - IMO's research: Sulphur and salinity measurements: Precipitation: SO4-S, NO3-N, Cl, Na, Mg, K, Ca (mg/l) Precipitation: conductivity (µS/cm), quantity (mm), pH Aerosol: SO4-S, Cl, Na, Mg, K, Ca, Fe (µg/m3) Air: SO2-S (µg/m3) Heavy metals in precipitation: Pb, Cd, Cu, Zn, Cr, Ni, Fe, Mn, V, As, Al (ng/ml) Cl, NO3-N, SO4-S, Na, K, Ca, Mg, NH4-N, Br, F (µg/ml) conductivity (µS/cm /pollution-and-radiation/pollution/components/

• 37. Kjellstrom_Erik_CES_2010

  ANN−10 −5 0 5 10 15 20 delta w (% ) 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17C h a n g e i n g e o s t r o p h i c w i n d s p e e d ( % ) Change in wind over the Baltic Sea in 70 years time at the time of CO2-doubling Chen and Aschberger, 2006 17 CM IP G CM s A need for regional ensemble simulations head2right Changes are uncertain head2right Size and sometimes even sign /media/ces/Kjellstrom_Erik_CES_2010.pdf

• 38. CASE_B__Heikki_Tuomenvirta_(FMI)_Introduction

  of climate change on the routine and periodic maintenance of roads. Helsinki 2009. Finnish Road Administration, Central Administration. Finnra reports 8/2009, 66 p. + app. 8 p. ISSN 1459-1553, ISBN 978-952-221-172-9, TIEH 3201122-v. (in Finnish, abstract in English) [5] Salanne, i., Byring, B., Valli, R., Tikkanen, R., Peltonen, P., Haapala, J., Jylhä, K., Tolonen-Kivimäki, O., and Tuomenvirta, H /media/loftslag/CASE_B__Heikki_Tuomenvirta_(FMI)_Introduction.pdf

• 39. VI_2017_009

  we take the corresponding data from the CMIP5 project. Table 1. All GCMs and RCMs used in this study. If a model is available for any of the domains Arctic-44, EURO-44, or EURO-11, it is marked with a v, but with an x if it is unavailable. Model name Type EURO-11 EURO-44 Arctic-44 CCCma-CanESM2 GCM x v v COSMO-CLM4-8-17 RCM v v x CNRM-CERFACS-CNRM-CM5 GCM v v x IHCEC-EC-Earth GCM v v v /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 40. VI_2009_012

  Mw(v) plotted against log distance. The coefficient of correlation between Mw(v) and log distance is 0.24. High correlation coefficients have been shown to affect parameter estimates in one step regression methods (see Fukushima and Tanaka, 1990). The Ci values were also calculated from the derived PGA values. Instead of constructing another magnitude scale based on acceleration it was decided /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf