58 results were found for WA 0852 2611 9277 Pemborong Interior Ruang Keluarga Kecil Apartemen Grand Lotus Residence Depok.

Results:

• 51. vanRoosmalen_etal-2009-WRR_2007WR006760

  that groundwater recharge is a function of the changes in the meteorological input based on the selected climate scenario in combination with landscape character- istics, e.g., soil types, land use, and depth to the water table and human impacts such as drainage, groundwater abstractions, and flow regulation. Jyrkama and Sykes [2007] showed that groundwater recharge in the Grand River watershed, Ontario /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 52. Hare-2011-ParticipatoryModelling

  ea th , th e m et ho d u se d at th is st ag e fo r th es e st ak eh o ld er typ es is sp ec i
  ed .Sh oul d ther e be tw o o r mor e model sbein g develope d in th e process ,the n th e typ e o fmode lt o whic h th e metho d wa s applie d is show n in parentheses .O T re fe rs to th e co m po si tio n o ft he o rg an iz in g te am . Fo r o rg an iz in g te am in vo lve m en t in di ffe re n t pa rt /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 53. 2010_016

  -based and 10 based on IPCC GCM simulations. The choice of the GCM models was based on their SAT performance for the present-day climate near Iceland as mentioned above. 2. For GCM-based scenarios, temperature change in the highland interior of Iceland, where the large ice caps are located, were increased by 25% based on the results of RCM downscaling (Nawri & Björnsson, 2010). 3. Expected /media/ces/2010_016.pdf

• 54. 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

• 55. Adalgeirsdottir-etal-tc-5-961-2011

  by 25 % in the interior of Ice- land, where the large ice caps are located (Nawri and Björns- son, 2010). Before year 2010, the glacier model is forced with daily mean records constructed from the monthly mean observed temperature and precipitation as previously explained. Pos- sible natural variations in the climate are important for near- future projections as the magnitude of the expected /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 56. GA_2009_91A_4_Andreassen

  Kjøllmoenet al. 2007).Storbreen is located just east of the main waterdivide between east and west in southern Norwayand receives precipitation from both directions(Liestøl 1967). The glacier is part of an east–west mass balance transect in southern Norway where mass turnover is largest near the western coast anddecreases towards the drier interior (Andreassen etal. 2005). Storbreen is in this respect /media/ces/GA_2009_91A_4_Andreassen.pdf

• 57. Kok_et_al._TFSC_published_2011

  is on aspects in which the method of linking exploratory scenarios and backcasting differed from the prevailing methodology. A complete overview of all results of the backcasting exercise can be found in [41]. 3.4.1. Total number of items A grand total of 243 actions, milestones, opportunities, and obstacles was dened, rather evenly spread among the four scenario groups (see Table 4). Of those /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

• 58. VI_2020_005

  glacier, and a general land rise along the southern coast and in the countries interior (figure 1). This rise results from recent melt of the Icelandic glaciers, which have been melting since the late 19th century. An acceleration in land uplift is even evident in the Southeast. STL analysis of vertical GPS measurements in 1997- 2015 from Höfn in Hornafjörður show over 8 mm/yr uplift in the first /media/vedurstofan-utgafa-2020/VI_2020_005.pdf