98 results were found for WA 0821 7001 0763 (FORTRESS) Pintu Baja Terbaru Long Pahangai Mahakam Hulu.

Results:

• 1. Kok_et_al._TFSC_published_2011

  development is well-suited to the challenges posed by the WFD to develop a long-term view by involving stakeholders. In this paper we analyse the process and results of a series of stakeholder workshops to develop scenarios at pan-European level. Specifically, we aim at analysing the method and results of combining a backcasting methodology and exploratory scenario development process. Four /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

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

  data. The pdfs, in turn, are used to evaluate and manage risks to water supplies, water- works, and floodplains; annual global invest- ment in water infrastructure exceeds U.S.$500 billion (1). The stationarity assumption has long been compromised by human disturbances in river basins. Flood risk, water supply, and water quality are affected by water infra- structure, channel modifications /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 3. IPPC-2007-ar4_syr

  of the permafrost layer have generally in- creased since the 1980s in the Arctic by up to 3°C. {WGI 3.2, 4.5, 4.6, 4.7, 4.8, 5.5, SPM} At continental, regional and ocean basin scales, numerous long- term changes in other aspects of climate have also been observed. Trends from 1900 to 2005 have been observed in precipitation amount in many large regions. Over this period, precipitation in- creased /media/loftslag/IPPC-2007-ar4_syr.pdf

• 4. 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

• 5. VI_2021_008

  Amplitude Measurement (RSAM) data are one of the most important tools utilized in volcano observatories worldwide. The IMO’s monitoring office is no exception, as this type of real-time data shows mid- to long-term trends, which is especially important for monitoring active volcanic systems. The RSAM methodology was developed by the USGS in 1989 (Murray & Endo, 1989) to plot averaged amplitude /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

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

  produc- tion) and multiple stakeholder platforms are therefore being suggested as an important design principle for river basin management at different scales (Pahl-Wostl et al. 2007b). Such an institutional design principle would be an addition to the design principles developed by Ostrom (1990), which are based on long enduring local and single- use common pool resource communities. In contrast /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 7. Journal_of_Hydrology_Veijalainen_etal

  - ferent parts of Europe. Both short-term and long-term estimates are needed for different planning time-horizons, since the changes in floods may not be linear. Hydraulic modelling has been the main tool for evaluation of flood inundation (Horritt and Bates, 2002; Hunter et al., 2007; Käyhkö et al., 2007; Pender and Néelz, 2007; Alho et al., 2008). The most common way of implementing the Floods /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 8. VI_2009_006_tt

  than can be expected to originate from the cauldrons, three to four times the wa- ter equivalent of the accumulation of snow over the watershed of the cauldrons. It has been estimated that flow from the cauldrons, in addition to the jökulhlaups, could be 2–5 m3 s 1 at maximum (Vatnaskil, 2005). It is possible that part of the sulfate-rich groundwater from the glacier comes from the cauldrons /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 9. Group4-Pres

  Policy practices 2 Policy itself 3 The policy making process 4 The positions and arguments held by advocates and opponents 5 The beliefs values and perspectives held by institutions, regimes, and interest groups 6 The broadly shared beliefs, values and perspectives (metacultural frames) typical to a societal culture IncreasedFreeze Thaw Cycles (Structural Technologies) Short – Long term /media/loftslag/Group4-Pres.pdf

• 10. Sea-ice observations last 30 days

  Sea-ice observations last 30 days Navtex message ICE REPORT 30 04 2023 AT 12:20 UTC SEA ICE OBSERVATION FROM A SHIP ICE STRIP 3 NM LONG AT 67:46.6N, 20:00.08W TO 67:46.4N, 19:51.0W EASILY SEEN IN RADAR ANOTHER STRIP VISIBLE NORTH /sea-ice/navtex