81 results were found for WA 0821 1305 0400 Biaya Borongan Interior Ruang Tamu Leter L Berpengalaman Ciledug Kota Tangerang.

Results:

• 1. VI_2015_007

  the report. 2 Study area and data 2.1 River basins The region under study is located in the East fjords and the surrounding area (Fig. 1). This region is characterised by a complex topography along the coast, Vatnajökull ice cap in the southwest and highlands in the interior. This leads to large precipitation and temperature gradients in the region (Crochet et al., 2007; Crochet & Jóhannesson, 2011). Eight /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

• 2. VI_2014_006

  (L), glacial rivers (J) and whether they flow through lakes (S). The combination of letters indicates the origin of flow with the first letter indicating the primary origin. The hydrological regime of these catchments is influenced by rainfall in autumn and winter, snowmelt in spring (and glacier melt in summer). 15 Table 1. Characteristics of the considered watersheds. Letter combinations indicate /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 3. VI_2013_008

  combinations indicate the type of river, with the first letter indicating the primary type. Direct runoff river (D), presence of lakes (S), glacier-fed river (J), groundwater (L). Gauging station vhm vhm vhm vhm vhm vhm 19 10 26 145 66 64 Name Dynjandisá Svartá Sandá Vestari- Hvítá Ölfusá Jökulsá Type of river D+L D+L D+L D+J+L L+J L+D+J+S Drainage area (km 2) 42 397 267 850 1664 5687 Mean altitude (m a.s.l /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 4. ESC-IASPEI-statement-LAquila-2012-1

  26 October 2012 ESC statement on L’Aquila sentence The European Seismological Commission (ESC) as a Commission of the International Association of Seismology and Physics of the Earth’s Interior (IASPEI) endorses and adheres to the IASPEI Press Release on the L'Aquila sentence (http://www.iaspei.org/news_items/laquila_IASPEI_press_release_final.pdf /media/vedurstofan/utgafa/hlidarefni/ESC-IASPEI-statement-LAquila-2012-1.pdf

• 5. VI_2015_009

  presents the study area and data. Sec- tion 3 describes the methodology. Section 4 presents the results and Section 5 concludes the report. 2 Study area and data 2.1 River basins Rivers in Iceland are often classified according to the origin of flow (Rist, 1990): direct runoff (D), spring-fed (L), glacier-fed (J) and whether they flow through lakes (S). Twelve river basins were selected for this study /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 6. VI_2014_001

  in km2, L the catchment perimeter in km, Z the catchment mean altitude in meters, P the catchment averaged mean annual precipitation in mm/day for the period 1971–2000 and Pm the catchment averaged mean annual maximum daily precipitation in mm/day for the period 1971–2000. 3.3 Evaluation statistics The evaluation of the index flood regression models (Eqs. 7 to 12) was first conducted by calcu /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 7. Milly_etal-2008-Stationarity-dead-Science

  6University of Washington, Seattle, WA 98195, USA. 7NOAA Geophysical Fluid Dynamics Laboratory, Princeton, NJ 08540, USA. *Author for correspondence. E-mail: cmilly@usgs.gov. An uncertain future challenges water planners. Published by AAAS on July 12, 201 1 www.sciencemag.or g Downloaded from 1 FEBRUARY 2008 VOL 319 SCIENCE www.sciencemag.org574 POLICYFORUM combined with opera- tions /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 8. VI_2014_005

  %) Subpolar wetlands: 7,208 km2 (7.5%) Subpolar crops: 2,380 km2 (2.5%) Inland water4: 1,463 km2 (1.5%) 4Including also the coastal lagoon Hópið, and the estuary at Höfn. 9 Inland Water Subpolar Wetlands Subpolar Crops Subpolar Pastures Tundra Sparse Tundra Permanent Snow Vatnajökull Mýrdalsjökull Langjökull Hofsjökull Drangajökull Eyja fjall ajö kul l Reykjanesskagi Sp ren gis an du r /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 9. IPPC-2007-ar4_syr

  /media/loftslag/IPPC-2007-ar4_syr.pdf

• 10. VI_2009_006_tt

  lake in a volcanic caldera in the interior of the Vatnajökull ice cap (Björns- son, 1988). Jökulhlaups from Grímsvötn have been known since at least the fourteenth century (Þórarinsson, 1939, 1974). In the beginning of the twentieth century there were about ten years between outbursts but the floods diminished with time and became more frequent. After a catastrophic, rapidly rising flood caused /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf