68 results were found for WA 0821 1305 0400 RAB Kanopi Model Modern Murah Cakung Jakarta Timur.

Results:

• 21. Journal_of_Hydrology_Veijalainen_etal

  in flooding were evaluated at 67 sites in Finland with var- iable sizes of runoff areas using a conceptual hydrological model and 20 climate scenarios from both glo- bal and regional climate models with the delta change approach. Floods with a 100-year return period were estimated with frequency analysis using the Gumbel distribution. At four study sites depicting dif- ferent watershed types /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 22. 2013_001_Nawri_et_al

  effects . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 19 4 Evaluation of model results 22 5 Large-scale overview 26 5.1 Climatological wind conditions . . . . . . . . . . . . . . . . . . . . . . . . . . . . 26 5.2 Wind power density . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 31 6 Test sites 36 7 Conclusions 41 A Resource maps 42 A.1 Blanda /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 23. VI_2009_013

  to Eyjafjallajökull. .... 11  Figure 3. Recorded seismicity by the SIL-system in Eyjafjallajökull and vicinity. ......... 13  Figure 4. Relocated seismicity using model P23-ave and model SIL .............................. 16  Figure 5. Selected relocated events with low relative error ............................................. 17  Figure 6. Temporal/spatial evolution of seismicity 1991–1995 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 24. VI_2009_006_tt

  –conduit model for subglacial water flow was used to simulate the jökulhlaup. The model was forced with the estimated outflow from the subglacial lake. The simulations were not successful as a realistic subglacial pressure field could not be obtained for a reasonable fit of the jökulhlaup discharge at the glacier terminus. This indicates that the physical basis of the model is insufficient to provide /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 25. VI_2017_009

  Vavrus et al. (2011) used simulations by NCAR’s Community Climate System Model, version 4 (CCSM4), the study of Nawri and Björnsson (2010) used various IPCC ensembles of GCMs simulations, and Koenigk et al. (2015) used the Coupled Model Intercomparison Project, Phase 5 simulations (CMIP5). According to Nawri and Björnsson (2010) the average temperature in Iceland will increase by +0.2°C /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 26. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 27. VI_2020_008

  bridges, and culverts. This dependency necessities a new analysis of precipitation extremes and a reassessment of precipitation return periods. The modern-day availability of high temporal frequency precipitation measurements, i.e. down to 10 minutes, at various locations around the country enables testing and refinement of the original 1M5 model. Moreover, there have been major advances /media/vedurstofan-utgafa-2020/VI_2020_008.pdf

• 28. 2010_003rs

  plate spreading motion, according to the NUVEL-1A plate motion model (DeMets et al., 1990, 1994). Using a simple screw dislocation model to interpret GPS campaign measurements on the RP from 1993 and 1998, Hreinsdóttir et al. (2001) suggested that rifting on the peninsula occurred in pulses, since their research indicated present accumulation of left-lateral shear strain parallel to the peninsula /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 29. VI_2020_005

  sinking. This was estimated from an assumed absolute sea level rise along with relative sea level trends. However, an underestimation of land uplift is probable in these assessments (Madsen, 2009). A land uplift model for Denmark produced by DTU Space with GNSS data from Geodatastyrelsen, precision levelling and the Danish Meteorological Institute’s water level data, shows land uplift of just under /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 30. VI_2021_008

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