73 results were found for WA 0859 3970 0884 Vendor Interior Rumah Minimalis Type 50 Lendah Kulon Progo.

Results:

• 51. Statistical Analysis

  & Hannah, D.M. (2010). Regional hydrological drought in north-western Europe: linking a new Regional Drought Area Index with weather types. Hydrological Processes , 24 (in press), doi: 10.1002/hyp.7644. Fleig, A., Tallaksen, L.M., Hisdal, H., Stahl, K. & Hannah, D.M. (2009). Inter-comparison of weather and circulation type classifications for hydrological drought development. Physics /ces/publications/nr/1943

• 52. Refsgaard_2-uncertainty

  from Walker et al. (2003) Source of uncertainty Level (type) of uncertainty Nature Statistical uncertainty Scenario uncertainty Qualitative uncertainty Ignorance Epistemic uncertainty Ontological uncertainty Ambiguity Inputs System data Driving forces Model Model structure Technical Parameters Context (boundary conditions) Future /media/loftslag/Refsgaard_2-uncertainty.pdf

• 53. Pilot reports

  conditions encountered by an aircraft in flight. This information is usually relayed by radio to the nearest ground station. At a minimum the PIREP must contain a header, aircraft location, time, flight level, aircraft type and one other field. All significant weather encountered by an aircraft in flight, either to or from any Icelandic airport or airstrip, shall be reported to the Icelandic /weather/aviation/pirep/

• 54. Outline of the earthquake fault in Ölfus

  of the earthquake fault in Ölfus 30.5.2008 The map shows the location of the damaging earthquake that struck yesterday afternoon. Most movement took place along the fault shown in green. The black arrows denote right-lateral, strike-slip faulting. The same type /about-imo/news/nr/1312

• 55. norsem_janutyte

  package. From the recorded data we obtained nearly 120 FPS of the earthquakes and assigned them with the quality factors. We grouped the earthquakes into several groups according to their geographical locations, and investigated the obtained results in each group separately. The overall results in the study area show the dominating normal type of faulting and the N-S /media/norsem/norsem_janutyte.pdf

• 56. Instructions for cloud cover forecasts

  The first map shows cloud cover measurements at a few stations in Iceland, along with information about cloud type and lowest cloud altitude (see following diagram). This information can be useful in evaluating the quality of the forecast. Cloud cover observations are made every three hours at a few stations in Iceland. The latest observation is shown /weather/articles/nr/1219

• 57. Map of the Glaciers of Iceland

  of the glaciers at their maximum at the end of the Little Ice Age (about 1890) and also at the end of the 20th century. On the map surge-type glaciers are distinguished from non-surge-type glaciers with a darker green color. A symbol shows volcanic calderas which are located underneath the glaciers. Also shown are place-names of all of the glaciers that have been given names. An explanatory /about-imo/news/nr/2712

• 58. ces_geus_paakitsoq_full_report

  22N) from till Illulisat DMI 50 10 105 497382 7681278 Ta 1.1.81 6.4.06 Station 437 ASIAQ 275 340 311 531316 7709513 Ta 5.9.83 1.6.06 Swiss Camp GC-net 1150 1115 780 566396 7719204 Ta, Sin 1.1.95 8.5.06 Crawford GC-net 2022 1795 1982 654464 7757807 Ta, Sin 24.5.95 2.5.06 2 2.3 RCM Data Output from two RCMs is used: (1) the regional coupled ocean-atmosphere model RCAO (Döscher et al., 2002) and (2 /media/ces/ces_geus_paakitsoq_full_report.pdf

• 59. 2010_016

  and the groundwater module. The coupling between both modules was done by a net boundary flux between the unsaturated zone and the groundwater (Schulla & Jasper, 2007). Information on land use, soil type, elevation and other general properties of the watershed are given in static distributed grids while a number of parameters describing specific processes are adjusted to the properties of each /media/ces/2010_016.pdf

• 60. VI_2016_006_rs

  was 0.1–0.2 C and the flow was 40–50 l/s (Árni Hjartarson, 2015). The inner Efri-Botnar area is similar to the outer cirque, but the thickness of the debris appears to be somewhat greater. There are ridges and lateral glacier moraines within the cirque and the thickness of the piles of loose materials near the mouth of the cirque is around 6–8 m. Glacier striations from the end of the last ice age can /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf