81 results were found for T 겟투더벳 cddc7.com ○보너스번호 B77○페르셀라 라몽간╽토토베이ൂ인천중구 원엑스벳⋛영광 공유방💉겟투더벳애용 circumlocutory/.

Results:

• 31. 2010_005_

  ensemble mean SAT values during the 1961–90 control period. The exact values of linear SAT trends, determined by least-squares regression, are given in Table 4. Based on a standard t-test, all these trends are significantly different from zero on the 99.9% confidence level. As seen before, based on the reduced IPCC ensemble mean, differences in linear SAT trends over the ocean and the land are small /media/ces/2010_005_.pdf

• 32. VED_AnnualReport-2013_screen

  and our intention is to run these models dur- ing times of hazardous events and even on a daily basis to further improve monitoring. Avalanche monitoring has progressed. The em- phasis is now on improving our services, especially to the Icelandic Road and Coastal Administration with regard to transport. The reason is that com- munity structure has changed considerably in recent years and the need /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

• 33. Paper-Olafur-Rognvaldsson_92

  a systematic com- parison of results to observed precipitation has been carried out. Un- dercatchment of solid precipitation is dealt with by looking only at days when precipitation is presumably liquid or by considering the occurrence and non-occurrence of precipitation. Away from non- resolved orography, the long term means (months, years) of observed and simulated precipitation are often /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 34. High resolution precipitation maps for Iceland

  maps for 1971-2000 Daily precipitation maps are available on request and further information on the making of the maps. IMO's contacts for this project are Philippe Crochet and Tómas Jóhannesson. Reference: Crochet, P., T. Jóhannesson, T. Jónsson, O. Sigurðsson, H. Björnsson, F. Pálsson and I. Barstad (2007): Estimating the spatial distribution of precipitation in Iceland using a linear model /weather/articles/nr/1625

• 35. Statistical Analysis

  and Chemistry of the Earth, Special Issue: COST Action (Accepted for publication). Jónsdóttir, J. F., Uvo, C. B. & Clarke, R. T. (2008). Filling gaps in measured discharge series with model-generated series. Technical Notes. Journal of Hydrological Engineering, 13, 9, 905-909. Jónsdóttir, J. F., Uvo, C. B. & Clarke, R. T. (2008). Trend analysis in Icelandic discharge, temperature and precipitation series /ces/publications/nr/1943

• 36. VI2010-006_web

  Veðurstofu Íslands Halldór G. Pétursson, Náttúrufræðistofnun Íslands H æ t t u matsnefnd Akureyrarbæjar 4 Efnisyfirlit 1 Inngangur 7 1.1 Starf hættumatsnefndar . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 7 1.2 Vinnuferli Veðurstofu Íslands . . . . . . . . . . . . . . . . . . . . . . . . . . . 7 1.3 Efnisatriði og kaflaskipting /media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf

• 37. Cradden_Lucy_CES_2010

  2050s 2080s C h a n g e i n r a t i n g ( % ) 10% 50% 90% C h a n g e i n r a t i n g ( % ) C h a n g e i n r a t i n g ( % ) Each bar shows range over whole UK spatial area June 2010 13 Is the impact similar over the whole UK? • Changes in the summer minimum rating, i.e. worst-case conditions – max temperature: Rating at baseline period 1961 /media/ces/Cradden_Lucy_CES_2010.pdf

• 38. Dyrrdal_Anita_CES_2010

  Results W i n t e r t e m p e r a t u r e Max snow depth Trend slope Number of snow days Period II P e r i o d I I I Max snow depth Number of snow days Norwegian Meteorological Institute met.no Correlation analysis (1961-08) 138 mutual stations Introduction Data & Methods Results Correlation with winter temperature Correlation with winter precipitation In warmer regions both snow parameters /media/ces/Dyrrdal_Anita_CES_2010.pdf

• 39. VI_2015_007

  maximum flow. For time periods, see Table 1. 10 3 Index flood method 3.1 General principle The method has already been described in detail in Crochet (2012a,b) and Crochet & Þórarins- dóttir (2014) and so is only summarised here. The index flood method (IFM), proposed by Dalrymple (1960) can be used to estimate the T -year flood quantile at ungauged locations or at gauged sites with short records /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

• 40. VI_2009_006_tt

  to theoretical framework. I do also want to thank him for an enjoyable time during this work, both in the office and in the field. This work was carried out as a part of the Skaftá cauldrons research project which was funded and supported by the Icelandic Centre For Research (RANNÍS), Kvískerja- sjóður, the NASA Astrobiology Institute, Landsvirkjun (the National Power Com- pany), the National Energy /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf