54 results were found for WA 0821 7001 0763 (FORTRESS) pintu baja lebar 80 cm Tlogomulyo Kabupaten Temanggung Jawa Tengah.

Results:

• 1. Kok_et_al._TFSC_published_2011

  17 24 64 Sustainability Eventually 5 3 30 28 66 Fortress Europe 18 11 30 23 72 Policy Rules 6 5 13 17 41 Total 44 27 80 92 243 844 K. Kok et al. / Technological Forecasting & Social Change 78 (2011) 835–851 Author's personal copy sector. The presence of various climate-related strategies is a consequence of the presence of climate-related obstacles and opportunities. 3.4.6. Robust elements Results /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

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

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

• 3. Journal_of_Hydrology_Veijalainen_etal

  The hydrological simulations were performed with the Wa- tershed Simulation and Forecasting System (WSFS) developed and operated in the Finnish Environment Institute (Vehviläinen et al., 2005). The WSFS is used in Finland for operational hydrolog- ical forecasting and flood warnings (www.environment.fi/water- forecast/), regulation planning and research purposes (Vehviläinen and Huttunen, 1997 /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 4. VI_2009_006_tt

  was therefore formed by ice lifting and deformation induced by subglacial water pressures higher than ice overburden pressure. The discharge data and the derived size of the subglacial flood path, as indicated by the volume of water stored subglacially, indicates a development towards more efficient subglacial flow over the course of the jökulhlaup. Thus, a discharge in the iii range 80–90 m3 s 1 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 5. 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

• 6. IPPC-2007-ar4_syr

  at higher northern latitudes (Figure 1.2). Average Arctic tem- peratures have increased at almost twice the global average rate in the past 100 years. Land regions have warmed faster than the oceans (Figures 1.2 and 2.5). Observations since 1961 show that the aver- age temperature of the global ocean has increased to depths of at least 3000m and that the ocean has been taking up over 80 /media/loftslag/IPPC-2007-ar4_syr.pdf

• 7. 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

• 8. Update on volcanic activity in Grímsvötn

  affecting the area around the crater. 26 May 2011 - 14:45 Yesterday, a group walked towards the eruptive site. Surveillance revealed much ash west and south of Grímsvötn. A few measurements, at locations where the ice was completely covered, gave ash thicknesses varying from 10 to 130 cm. Photo by Vilhjálmur Kjartansson, 25. maí 2011: 25 May 2011 - 18:05 Collective status report (pdf 35 Kb /earthquakes-and-volcanism/articles/nr/2180

• 9. Sitemap

  Sitemap | Observations | Icelandic Meteorological office Invalid parameter 'g'. Its value is: 80/ but should be an integer. Sitemap Front page Text forecasts | Station forecasts | El. forecasts | Observations Large quakes | Latest quakes | © IMO - Bústaðavegur 9 | 150 Reykjavík | Tel: 522 6000 /m/observations/areas

• 10. Factsheet_Bardarbunga_20141203

  to subsidence up-to 80 cm a day, but the subsidence has since slowed and it is now around 25 cm per day. The subsidence is in the shape of a bowl and it is greatest in the centre of the caldera, about 50 m, but smaller to the edges. o Crustal deformation: Extensive ground deformation Major was recorded while the dyke was forming, signalling the progression of the dyke and subsidence towards /media/jar/Factsheet_Bardarbunga_20141203.pdf