48 results were found for WA 0821 7001 0763 (FORTRESS) Pintu Rumah Cluster 1 Berkualitas Juhar Karo Sumatera Utara.

Results:

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

  ORIGINAL ARTICLE Climate change adaptation in European river basins Patrick Huntjens • Claudia Pahl-Wostl • John Grin Received: 1 July 2008 / Accepted: 24 December 2009 / Published online: 2 February 2010  The Author(s) 2010. This article is published with open access at Springerlink.com Abstract This paper contains an assessment and stan- dardized comparative analysis of the current water man /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 22. Bárðarbunga 2014 - August events

  the event than in the previous eruption, but more lava is being extruded. At 07 AM the lava flow was around 1 km wide and 3 km long towards northeast. The thickness was estimated a few meters, the flow about 1000 m3 pr second. Approximately 500 earthquakes were detected in the area and smaller than before. The strongest earthquake, M3.8 was in the Bárðarbunga caldera. Poor weather conditions prevail /earthquakes-and-volcanism/articles/nr/3000

• 23. Bardarbunga-2014_August-events

  It was detected on Míla´s web-camera at 05:51 AM. Fewer earthquakes seem to follow the event than in the previous eruption, but more lava is being extruded.  At 07 AM the lava flow was around 1 km wide and 3 km long towards northeast. The thickness was estimated a few meters, the flow about 1000 m3 pr second.  Approximately 500 earthquakes were detected in the area and smaller than before /media/jar/Bardarbunga-2014_August-events.pdf

• 24. Bárðarbunga 2014 - August events

  the event than in the previous eruption, but more lava is being extruded. At 07 AM the lava flow was around 1 km wide and 3 km long towards northeast. The thickness was estimated a few meters, the flow about 1000 m3 pr second. Approximately 500 earthquakes were detected in the area and smaller than before. The strongest earthquake, M3.8 was in the Bárðarbunga caldera. Poor weather conditions prevail /earthquakes-and-volcanism/articles/nr/3000/

• 25. 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

• 26. VI_2013_006

  lightning strikes can be over 10 km in length and are sometimes tilted and to the side of the volcanic column must be taken into account. This adds to the lightning location uncertainty, which is often a few km. Furthermore, the volcanic column may be swayed downwind, e.g. see Figure 1. Therefore, location of a single lightning can be misleading but by calculating average location of many /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_006.pdf

• 27. AnneFleig_May2010_CES

  Regional hydrological droughts in north-western Europe and associated weather types Anne K. Fleig (1), Lena M. Tallaksen (1), Hege Hisdal (2) & David M. Hannah (3) (1) University of Oslo, (2) Norwegian Water Resources and Energy Directorate, (3) University of Birmingham. CES conference, Oslo, Norway, 31 May - 2 June 2010 Bewl Reservoir in southeast England, February 2006. (Photo: Reuters /media/ces/AnneFleig_May2010_CES.pdf

• 28. IPPC-2007-ar4_syr

  Assessment Re- port (AR4). Topic 1 summarises observed changes in climate and their ef- fects on natural and human systems, regardless of their causes, while Topic 2 assesses the causes of the observed changes. Topic 3 pre- sents projections of future climate change and related impacts un- der different scenarios. Topic 4 discusses adaptation and mitigation options over the next few decades /media/loftslag/IPPC-2007-ar4_syr.pdf

• 29. Further information on the seismicity in Northern Iceland

  were M 3.6 at 03:42 and M 3.2 at 07:47. Since the afternoon of 23 October, a new cluster of earthquakes has occurred about 5 km north-northwest of Gjögurtá on the intersection of the eastern end of Eyjafjarðaráll and the Húsavík-Flatey Fault (HFF). The largest events in this region were M 3.1 at 23:38 on 23 October and 3.2 at 22:20 on 24 October (see the map). Movements on the fault of the M /about-imo/news/nr/2561

• 30. VI_2021_008

  -time and detects signal characteristics similar to previously observed eruptions using a three-fold detection procedure based on: 1) an amplitude threshold; 2) the signal-to-noise ratio; and 3) an emergent ramp-like shape. Data from six Icelandic eruptions was used to assess and tune the module, which can provide 10–15 minutes of warning for Hekla up to over two hours of warning for some other /media/vedurstofan-utgafa-2021/VI_2021_008.pdf