74 results were found for WA 0852 2611 9277 Perusahaan Kontraktor Interior Ruang Apartment B Residence BSD Tangerang.

Results:

• 11. Journal_of_Hydrology_Veijalainen_etal

  in Finland Noora Veijalainen a,*, Eliisa Lotsari b, Petteri Alho b, Bertel Vehviläinen a, Jukka Käyhkö b a Freshwater Centre, Finnish Environment Institute, Mechelininkatu 34a, P.O. Box 140, FI-00251, Helsinki, Finland b Department of Geography, FI-20014 University of Turku, Turku, Finland a r t i c l e i n f o Article history: Received 7 January 2010 Received in revised form 13 June 2010 Accepted /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 12. 2010_005_

  scenario, precipitation increased by 10–15% from 1961–90 to 2070–99, and by 5–10% for the lower emitting scenarios (corresponding to approximately 0.5–1% per decade). The CE project also examined RCM results for Iceland based on the HIRHAM model (Haugen and Iversen, 2006). These results showed enhanced warming over the interior of Iceland compared with the coastal zone, and a tendency for enhanced /media/ces/2010_005_.pdf

• 13. Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication

  their audience. Climatic Change (2012) 112:233–242 DOI 10.1007/s10584-011-0205-7 C. S. Weiler (*) Office for Earth System Studies, Whitman College, Walla Walla, WA 99362, USA e-mail: weiler@whitman.edu J. K. Keller School of Earth and Environmental Sciences, Chapman University, Orange, CA 92866, USA C. Olex The Point, 121 Jewett Street, Newton, MA 02458, USA 1 Introduction Of all the applications /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf

• 14. 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

• 15. VI_2020_011_en

  ........................................................................................................................ 56 APPENDICES ......................................................................................................................... 60 A. DEM, bathymetry, and topography ............................................................................... …60 B. Input parameters used to run the mrlavaloba simulations ............................................. …61 C /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 16. Energy Systems

  Publications and presentations Energy Systems Other international Mo, B., Doorman, G., Grinden, B., Henning, D /ces/publications/nr/1937

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

  ). Locations of the weather sta- tions, used to reconstruct the temperature and precipitation records, are shown with letters: Reykjavík (R), Fagurhólmýri (F), Hæll (H), Stykkishólmur (S), Teigarhorn (T), Vestamannaeyjar (V), Akureyri (A) and Hólar in Hornafjörður (HH). (B) The surface topography of Vatnajökull ice cap. Dots show the sites of mass balance and veloc- ity measurements, blue dots show /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 18. CES_D2.4_task1

  use a method developed by Räisänen and Ruokolainen (2008a,b) for this purpose; more details are provided in Section 2 and in the appendices of this report. The resulting best- estimate distribution for the year 2010 (red line) shows a higher probability of mild Decembers, and a lower probability of cold Decembers, than either of the two directly observation-based distributions. This estimate /media/ces/CES_D2.4_task1.pdf

• 19. VI_2015_007

  The idea is to compensate for the lack of temporal data by spatial data, taken within a homogeneous region with respect to flood characteristics, and transfer information regarding flood characteristics from gauged sites to the target site. The IFM has already been evaluated in northern Iceland (Crochet, 2012a,b). Results are very encouraging but indicate that a limited number of gauged sites can /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

• 20. Staff members

  Staff members Gunnar B. Guðmundsson Job title: Seismic System Scientist /about-imo/employees/persona/25/fyrirtaeki/2