40 results were found for WA 0821 7001 0763 (FORTRESS) pintu baja double Elar Kabupaten Manggarai Timur Nusa Tenggara Timur.

Results:

• 21. ved-eng-2010

  ) and Akureyri (red) expressed as percentage of the 1961 to 1990 base period. In Reykjavík the total was considerably below the normal in most months, except in January and September. The precipitation in Akureyri was unusually unevenly distributed during the year. There was almost no precipitation in January and June, but double the normal in February. There was also much precipitation /media/vedurstofan/utgafa/skylduskil/ved-eng-2010.pdf

• 22. Group2-report

   the opportunity to achieve  not only single, but double, and maybe even triple loop learning, which is key to adaptive management.       /media/loftslag/Group2-report.pdf

• 23. Henriksen-AM

  to poor responses to drought and low flow problems, a higher level of AIWM seems to result in more adequate responses to flood problems, at least in terms of flood protection or mitigation measures – AIWM enables more diversity in response measures => moving up in learning level (single -> double -> tripple) Responsivenes to droughts and floods (Huntjens et al., 2010) • Adaptation refers to both /media/loftslag/Henriksen-AM.pdf

• 24. VI_2009_013

  ................................................................. 30  9 1 Abstract Between 1991 and August 2006, 860 earthquakes in Eyjafjallajökull volcano, South Iceland were recorded by the SIL national seismic network. These earthquakes have been relocated using a relative, double-difference location method and their source mechanisms recalculated. The spatial and temporal seismicity pattern is analysed, as well as the distribution of focal /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 25. 2010_003rs

  to “bookshelf” type faulting. In June 2000, two large earthquakes of magnitudes ML6.4 and ML6.5 struck in the SISZ, three and a half days and approximately 17 km apart. Seismicity greatly increased in all Southwest Iceland and during 2000, roughly nineteen thousand microearthquakes were recorded there. The aim of this research is to relocate the earthquakes using a double- difference relative /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 26. Group4

  One of the key innovative features of this approach is the integration of a scaled (single/double/triple) helical learning model that embeds adaptive management principles. This creates the potential for the evolution of institutions to respond to changing socio-technical regimes. (Jaroszweski, Chapman, & Petts, 2010) Finally, a set of robust policy measures and strategies for adaptive /media/loftslag/Group4.pdf

• 27. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  the transition to adaptive water management regimes. 4.4. How can BNs support the transition from the currently prevailing regimes of river basin water management into more adaptive regimes that are better able to deal with changing conditions? It takes some effort to explain what we mean by this question to the water managers. To give an example of how we understand AM, we use the double loop learning /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 28. 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

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

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

• 30. 2005EO260001

  im- proved by a double-difference location meth- od [Slunga et al., 1995], and supported by P - wave particle-motion analysis at GRF, reveal a northerly trending event distribution, centered at the southern caldera rim, ~1 km east of the main eruption site (Figure 1b). Focal depths mostly concentrate above 4 km and decrease by ~2 km near the eruption onset. The detection threshold /media/jar/myndsafn/2005EO260001.pdf