33 results were found for WA 0821 7001 0763 (FORTRESS) Pintu Baja Putih Iv Koto Agam.

Results:

• 21. Refsgaard_2-uncertainty

  types: National database (DJF) • Precipitation: DMI’s 10 km grid daily values • Temperature, potential evapotranspiration: DMI’s 20 km grid Model calibration/validation (1990-2006) • 183 discharge stations, daily values • > 10,000 wells with groundwater head observations Change in groundwater head and discharge Skjern Å -20 -10 0 10 20 30 40 J F M A M J J A S O N D Måned R el at iv æ n d ri n g /media/loftslag/Refsgaard_2-uncertainty.pdf

• 22. 2010_017

  m J M5 [C°] -3 obs. [C°] -4 nce 1 re 5. Comp 26); an int temperatu this system y gridded v picion abo -Jökulsá w similar dif han observ h elevation ces the effe months No ly only on high the tem n band wi refore be s onthly tem an Feb Ma .2 -3.1 -3. .3 -4.1 -3. .1 1.0 0.6 arison of m erpolation re is shown atic differe alues, see T ut the qual atershed; b ference wa ations for t gradient fo /media/ces/2010_017.pdf

• 23. VI_2021_008

  /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

• 24. Journal_of_Hydrology_Veijalainen_etal

  The hydrological simulations were performed with the Wa- tershed Simulation and Forecasting System (WSFS) developed and operated in the Finnish Environment Institute (Vehviläinen et al., 2005). The WSFS is used in Finland for operational hydrolog- ical forecasting and flood warnings (www.environment.fi/water- forecast/), regulation planning and research purposes (Vehviläinen and Huttunen, 1997 /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 25. VI_2015_007

  and validation periods ....................................................................... 35 Appendix III - Instantaneous index flood µi(D = 0), flood frequency distribution and growth curves, derived by QDF modelling of WaSiM daily flow simulations ... 41 Appendix IV - Estimated flood frequency distributions at target sites treated as ungauged, using the best IFM for each set /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

• 26. VI_2020_004

  ....................................................................................... 99 APPENDIX I. Daily tephra dispersal simulation .................................................................... 102 APPENDIX II. HEKLA 1980 – The likelihood of receiving tephra at different locations .... 104 APPENDIX III. KATLA 1918 – The likelihood of receiving tephra at different locations ... 107 APPENDIX IV. ÖRÆFAJÖKULL 1362 /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 27. VI_2017_009

  /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 28. CES_D2.4_task1

  NO +62:34:01 +11:23:00 628 TP 1041 KONGSBERG IV NO +59:39:47 +09:39:00 168 TP 1042 LYNGOR FYR NO +58:38:00 +09:09:01 4 T 1043 TVEITSUND NO +59:01:37 +08:31:14 252 TP 1044 LINDESNES FYR NO +57:58:59 +07:02:53 13 TP 1045 LISTA FYR NO +58:06:36 +06:34:05 14 TP 1046 SOLA /media/ces/CES_D2.4_task1.pdf

• 29. Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games

  The instructions are provided in Appendix. In each session, participants were randomly assigned to a computer. The instructions told participants that they would take part in four different games: (i) Holt and Laury’s (2002) lottery, (ii) a modified dictator game, (iii) an ultimatum game, and (iv) the sequential public good game. Subjects did not know which type of game they were to play. They first /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf

• 30. Reykholt-abstracts

  1998 by the Electromagnetic system (EMI) of the Technical University of Denmark, iii) two image pairs from the SPOT 5 high resolution stereoscopic (HRS) instrument from August 2004 and iv) airborne lidar from August 2010 (after the Eyjafjallajökull eruption from 14 April to 22 May 2010). The average specific mass balance was estimated as the mean elevation difference between glaciated areas /media/vatnafar/joklar/Reykholt-abstracts.pdf