74 results were found for WA 0821 1305 0400 Kontraktor Hidroseeding Land Scaping Hijau Gunung Mas Kalimantan Tengah.

Results:

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

  drainage works, and land-cover and land-use change. Two other (sometimes indistinguishable) challenges to stationarity have been exter- nally forced, natural climate changes and low-frequency, internal variability (e.g., the Atlantic multidecadal oscillation) enhanced by the slow dynamics of the oceans and ice sheets (2, 3). Planners have tools to adjust their analyses for known human distur- bances /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 2. 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

• 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. 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

• 5. Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons

  296 Public Choice (2010) 143: 293–301 2 The commons The literature on the commons, or what is more technically defined as common-pool re- sources (CPRs), should be viewed initially from its place in the larger literature on dilem- mas of collective action. Since the foundational work of H. Scott Gordon (1954) on the com- mons, and Mancur Olson (1965) on collective action more broadly, the behavioral /media/loftslag/Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons.pdf

• 6. Sea ice in December 2010

  was closest to land 21.7 nm from Horn, 25.3 nm from Straumnes and 43.6 nm from Barði. The tongue which stretched eastwards, north of Iceland, was scattered. Only towards the west, the ice was quite dense. Large icebergs were seen in the area. On the 10th, IMO issued a warning saying that the ice edge might move closer to land in the next 24 hrs. The Coast Guard did an ice survey flight on the 12th /sea-ice/monthly/2010/nr/2347

• 7. Sea ice in August 2009

  in the period 6th to the 22nd, eight from ships and one from land. The icebergs were closest to land at 66°28,81'N og 21°23,86'V and close to Selsker (66°07,5N og 21°31'V). No seaice was in the Greenland Strait in August and northeasterly winds prevailed in the area /sea-ice/monthly/2009/nr/2330

• 8. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  Red indicates (a) airborne radar altimetry observed seasonally from 2004 to 2007, (b) the line of seasonal Ice, Cloud, and Land Elevation Satellite (ICESat) laser elevation data used in this study, observed from 2004 to 2007 and (c) global positioning system (GPS) profiles and sparse GPS observations at ice-free areas. Blue in (a
  d) indicates the ice cap margins. S. Gudmundsson et al. Mass balance /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

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

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

• 10. Journal_of_Hydrology_Veijalainen_etal

  Fin- land their unique characteristics. Topography, soil types and land use follow approximately the same distribution, with hilly till cov- ered areas in the north, flat clay agricultural areas near the coast and forested till areas with lakes in central Finland. Hydrology in Finland is characterized by strong snow-domi- nated seasonality with snow accumulation in winter and snow melt in spring /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf