56 results were found for 99贵宾汇开户(3266-409-932薇Q).adw.

Results:

• 11. VI_2014_005

  F., and Desroziers, G. (2011). Background-error covariances for a convective-scale data-assimilation system: AROME – France 3D-Var. Q. J. R. Meteorol. Soc., 137:409–422. Champeaux, J. L., Masson, V., and Chauvin, F. (2005). ECOCLIMAP: a global database of land surface parameters at 1 km resolution. Meteorol. Appl., 12:29–32. de Rosnay, P., Carver, G., Vitart, F., Balsamo, G., Wedi, N., Dutra, E /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 12. Journal_of_Hydrology_Veijalainen_etal

  be amplified by the RCM (Kjellstöm and Lind, 2009). Kjellstöm and Lind (2009) found that a systematic wet bias of 10–15% in precip- itation of the ECHAM5 GCM was increased to 20–30% in the RCM Table 1 Selected example areas for closer evaluation of climate change impacts on flood discharges and flood inundation area extents. Q is discharge and WSE water surface elevation. Map Ref. Fig. 1c Q gauge /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 13. Glossary

  We are hoping to find time to improve this glossary. Only a few items are available. For your relevant search, please click on one of the letters below: A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö A A: Icelandic abbreviation of East (compass direction, easterly, eastern). ANA: Icelandic abbreviation of Eastnorthesast (compass direction). ASA: Icelandic /weather/articles/nr/1208

• 14. Glossary

  We are hoping to find time to improve this glossary. Only a few items are available. For your relevant search, please click on one of the letters below: A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö A A: Icelandic abbreviation of East (compass direction, easterly, eastern). ANA: Icelandic abbreviation of Eastnorthesast (compass direction). ASA: Icelandic /weather/articles/nr/1208/

• 15. event_numbers_17022015

  Earthquakes since 16. August 2014 00:00 all intrusion caldera Kistufell Askja HB / HBT TFJ Kverkfj. automatic ~ 35.000 - - - - - - - checked ~ 20.000 ~ 8.000 ~ 9.000 ~ 200 ~ 300 ~ 1.800 ~ 600 ~ 20 M3.0-3.9 1208 99 1089 6 2 4 7 1 M4.0-4.9 655 7 646 1 1 0 0 0 M>5.0 79 0 79 0 0 0 0 0 HB / HBT Herðubreið and Herðubreiðartögl TFJ Tungnafellsjökull Kverkfj. Kverkfjöll Kistufell cluster north /media/jar/myndasafn/frodleikur/event_numbers_17022015.pdf

• 16. event_numbers_01102014_1500

  Earthquakes between 16. August 2014 00:00 and 01. October 2014 15:00 all intrusion caldera Kistufell Askja HB / HBT TFJ Kverkfj. automatic ~ 25.000 - - - - - - - checked ~ 8.500 ~ 5.500 ~ 1.600 ~ 120 ~ 250 ~ 850 ~ 130 ~15 M3.0-3.9 260 99 148 6 2 3 1 1 M4.0-4.9 83 7 74 1 1 0 0 0 M>5.0 39 0 39 0 0 0 0 0 HB / HBT Herðubreið and Herðubreiðartögl TFJ Tungnafellsjökull Kverkfj. Kverkfjöll Kistufell /media/jar/event_numbers_01102014_1500.pdf

• 17. event_numbers_07102014_1800

  Earthquakes between 16. August 2014 00:00 and 07. October 2014 18:00 all intrusion caldera Kistufell Askja HB / HBT TFJ Kverkfj. automatic ~ 26.000 - - - - - - - checked ~ 8.900 ~ 5.600 ~ 1.800 ~ 120 ~ 250 ~ 950 ~ 135 ~15 M3.0-3.9 307 99 195 6 2 3 1 1 M4.0-4.9 117 7 108 1 1 0 0 0 M>5.0 45 0 45 0 0 0 0 0 HB / HBT Herðubreið and Herðubreiðartögl TFJ Tungnafellsjökull Kverkfj. Kverkfjöll Kistufell /media/jar/event_numbers_07102014_1800.pdf

• 18. event_numbers_31102014_1900

  Earthquakes between 16. August 2014 00:00 and 31. October 2014 19:00 all intrusion caldera Kistufell Askja HB / HBT TFJ Kverkfj. automatic ~ 28.000 - - - - - - - checked ~ 11.900 ~ 6.500 ~ 3.550 ~ 140 ~ 260 ~ 1.200 ~ 250 ~15 M3.0-3.9 434 99 321 6 2 3 2 1 M4.0-4.9 228 7 219 1 1 0 0 0 M>5.0 61 0 61 0 0 0 0 0 HB / HBT Herðubreið and Herðubreiðartögl TFJ Tungnafellsjökull Kverkfj. Kverkfjöll /media/jar/event_numbers_31102014_1900.pdf

• 19. VI_2013_008

  types and for which daily discharge (Q) was available for at least thirty years was selected (Figure 1). Table 1 presents information on the characteristics of each catchment. Rivers in Iceland are usually classified according to their source (Rist, 1990; Jónsdóttir et al., 2008), namely direct runoff (D), groundwater fed (L), glacial rivers (J) and whether they flow through lakes (S). The combination /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 20. GA_2009_91A_4_Andreassen

  Fokstugu was used, r was 0.882. The differ- ence in r for the two periods is only 0.015 and doesnot indicate a systematic shift in summer tempera-ture due to the change in station location. Mass balance modelThe mass balance model calculates the mass bal- ance, b(z), as the sum of ablation and solid precip-itation: where Q is energy available for melt, Lm is latentheat of melting and Psolid /media/ces/GA_2009_91A_4_Andreassen.pdf