58 results were found for q 계산노래방х「zzan1.com》 계산노래주점 계산노래주점 계산레깅스룸◎계산2부집♘계산2부가게.

Results:

• 1. VI_2015_009

  vhm145 Vestari-Jökulsá D+J+L 844 751 11.3 924 1971–2014 vhm167 Austari-Jökulsá D+J 553 916 28.8 1208 1985–2014 8 vhm59 vhm64 vhm66 vhm102 vhm116 vhm162 vhm233 vhm235 vhm238 vhm144 vhm145 vhm167 Figure 1. Location of river basins. 9 l l l l l l l l l l l l l l l l l l ll l l l l l l l l l l l l l ll l l l l l 0 100 200 300 50 15 0 25 0 35 0 Days since Sept. 1st Q (m ³/s ) vhm59 S O N D J F M A M J /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 2. Kriauciuniene_Jurate_CES_2010

  of temperature anomaly (ºC) between 1991-2007 and 1961-1990 Variation of annual T anomaly (ºC) between 1991-2007 and 1961-1990 Seasonal differences of P anomaly (in %) between 1991-2007 and 1961-1990 Seasonal differences of Q anomaly (in %) between 1991-2007 and 1961-1990 Variation of annual P and Q anomaly (%) between 1991-2007 and 1961-1990 -40 -25 -10 5 20 35 50 1 9 2 0 1 9 4 0 1 9 6 /media/ces/Kriauciuniene_Jurate_CES_2010.pdf

• 3. ces_SA_group_flyer_new

  series analysis Regional series are compiled based on regions having similar climatological characteristics and streamflow regimes. These series are also useful for evaluating patterns and trends, both in time and by region. Regional series for precipitation, temperature and runoff are being compiled, updated and analysed within the CES project. - 4 0 - 2 0 0 2 0 4 0 6 0 W S P S U M A Q , % - 4 0 /media/ces/ces_SA_group_flyer_new.pdf

• 4. VI_2015_007

  study and location of catchments. Catchment vhm278 is embedded within vhm148 and catchment vhm277 is embedded within vhm149. 9 l l l l l l ll l l l l l l l l l l l l ll l l l l l l ll l ll l l l l l l 0 100 200 300 10 0 20 0 30 0 40 0 Day since 1st Sept. Q m³ /s VHM 148 S O N D J F M A M J J A l l ll l l l ll l l l ll l l ll l l 0 100 200 300 15 0 25 0 35 0 45 0 Day since 1st Sept. Q m³ /s VHM /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

• 5. VI_2014_001

  the index flood µi(D). For gauged sites, µi(D) is estimated by the sample mean whereas for ungauged sites, µi(D) is estimated indirectly as a function of physiographic and climatic catchment characteristics (Ci;k): bµi(D) = f (Ci;k);k = 1;n: (2) This estimation is usually performed using the power-form equation: bµi(D) = q0C q1 i;1C q2 i;2::::C qk i;k:::C qn i;n: (3) where q denotes the vector /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 6. 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

• 7. 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/

• 8. Journal_of_Hydrology_Veijalainen_etal

  ; 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

• 9. 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

• 10. GA_2009_91A_4_Andreassen

  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