16 results were found for WA 0821 1305 0400 RAB Paving Anti Lumut Segi 6 Bogor Barat Kota Bogor.

Results:

• 1. Kok_JGEC658_2009

  in the models, while on the other hand, models require quantitative information on a wealth of parameters that is often difficult to extract from storylines. In other words, there is a mismatch between storylines and model parameters (Steps 3–4 in Fig. 1), as well as between model output and revised stories (Steps 5–6). In practice, particularly the translation of stories into quantified model /media/loftslag/Kok_JGEC658_2009.pdf

• 2. Kok_and_Veldkamp_editorial_ES-2011-4160

  Tengö, D. Timmer, and M. Zurek. 2007. Linking futures across scales: a dialog on multiscale scenarios. Ecology and Society 12(1): 17. [online] URL: http://www.ecolog yandsociety.org/vol12/iss1/art17/. Borgatti, S. P., and P. C. Foster. 2003. The network paradigm in organizational research: a review and typology. Journal of Management 29(6):991-1013. Brenner, N. 2001. The limits to scale /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf

• 3. Isskyrsla_20101212

  örugt að fara fyrir Horn í um 10 sml frá landi en það yrði að hafa góðan útvörð. Kl.1341, kalla TFB og spyr um ETA í RVK, ETA um kl 1440. Kl 1305, AIS umferð fyrir N- Horn. Vegna bilunnar í WS 1 var megináhersla lögð á ískönnun í þessu flugi. Flugskýrsla TF-SIF 12. desember 2010 Flug nr. 117410.025 Ískönnun. Meginröndin lá um eftirtalda staði. 1. 67°47.0N 023 /media/hafis/skyrslur_lhg/Isskyrsla_20101212.pdf

• 4. 2005EO260001

  Dashed lines encompass the V-shaped zone of tephra deposition. (c) Oblique aerial view from west of the tephra plume at Grímsvötn on 2 November. Note the ashfall from the plume. (Photo by M. J. Roberts.) (d) Weather radar image at 0400 UTC on 2 November. The top portion shows its projection on an EW-vertical plane. The minimum detection height for Grímsvötn is seen at 6 km, and the plume extends /media/jar/myndsafn/2005EO260001.pdf

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

  This increases precipitation, and possibly flood risk, where prevailing atmo- spheric water-vapor fluxes converge (6). Rising sea level induces gradually height- ened risk of contamination of coastal fresh- water supplies. Glacial meltwater temporar- ily enhances water availability, but glacier and snow-pack losses diminish natural sea- sonal and interannual storage (7). Anthropogenic climate warming /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

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

  The Netherlands 123 Reg Environ Change (2010) 10:263–284 DOI 10.1007/s10113-009-0108-6 On a global scale, the number of disasters caused by weather-related phenomena such as storms, floods, and droughts has more than doubled over the past decade, from 175 in 1996 to 391 in 2005 (IFRC 2008). The same trend (Fig. 1) is being observed in the case-studies under inves- tigation, which is Rivierenland /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 7. IPPC-2007-ar4_syr

  and their interactions with sustainable develop- Figure I.1. Schematic framework representing anthropogenic drivers, impacts of and responses to climate change, and their linkages. Schematic framework of anthropogenic climate change drivers, impacts and responses ment. Topic 5 assesses the relationship between adaptation and mitigation on a more conceptual basis and takes a longer-term per- spective. Topic 6 /media/loftslag/IPPC-2007-ar4_syr.pdf

• 8. Eriksson_Garvill_Nordlund_2006

  Eriksson et al. / Journal of Environmenta in own car use, expected consequences for own freedom to choose travel mode, and acceptability. 2.3. Index variables Items measuring pro-environmental orientation and problem awareness were combined into index variables. First, the seven statements expressing an anti-NEP position were reversed so that higher values on all items reflected stronger NEP /media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf

• 9. 2010_017

  ............................................................................................................................... 5 TABLES ................................................................................................................................. 6 1 ABSTRACT ..................................................................................................................... 7 2 INTRODUCTION /media/ces/2010_017.pdf

• 10. Journal_of_Hydrology_Veijalainen_etal

  to increase in Finland by 13–26% by the 2080s (Ruosteenoja and Jylhä, 2007) and extreme precipitations are expected to in- crease (Beniston et al., 2007). On the other hand, temperature in- creases of 2–6 C by the end of the century are estimated to decrease the snow accumulation by 40–70% by the same period (Vehviläinen and Huttunen, 1997; Beldring et al., 2006; Ruosteeno- ja and Jylhä, 2007 /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf