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59 results were found for Q 선불폰팅《www-7982-me》 서울중구폰팅 서울중구채팅φ서울중구상황극Ⓗ연인폰팅 ぃ傊 maharani.


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  • 1. 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
  • 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_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
  • 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. VI_2020_008

    a precipitation value from a given location based on values from a regular gridded dataset. ................................................................................................. 28 Figure 7. Scatterplots and QQ plots comparing daily precipitation from the ICRA dataset and observations with different extraction methods for station Eskifjörður. .................................. 30 /media/vedurstofan-utgafa-2020/VI_2020_008.pdf
  • 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. 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/
  • 9. VI_2013_008

    of the analogue method is introduced. In Section 3 hydrological and me- teorological data used in the analysis are presented. Section 4 describes the different strategies considered for implementing the method and Section 5 presents some results. Some concluding remarks are made in Section 6. 2 The analogue method Let X(t) be a state of a dynamical system at time t, known through the observation of k variables /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf
  • 10. VI_2014_006

    of the deterministic forecast were measured by the mean error (ME), root-mean squared error (RMSE) and Nash-Sutcliffe coefficient (Nash and Sutcliffe, 1970). 3 Data 3.1 Meteorological data Predictors: Mean sea level pressure (MSLP), geopotential height (Z), specific humidity (q) and tem- perature (T) at different pressure levels constitute the predictors describing the meteoro- logical situations at synoptic /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

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