73 results were found for WA 0859 3970 0884 Vendor Interior Rumah Minimalis Type 50 Lendah Kulon Progo.

Results:

• 1. Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication

  Personality type differences between Ph.D. climate researchers and the general public: implications for effective communication C. Susan Weiler & Jason K. Keller & Christina Olex Received: 27 August 2009 /Accepted: 28 July 2011 / Published online: 2 September 2011 # The Author(s) 2011. This article is published with open access at Springerlink.com Abstract Effectively communicating the complexity /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf

• 2. ESC-IASPEI-statement-LAquila-2012-1

  26 October 2012 ESC statement on L’Aquila sentence The European Seismological Commission (ESC) as a Commission of the International Association of Seismology and Physics of the Earth’s Interior (IASPEI) endorses and adheres to the IASPEI Press Release on the L'Aquila sentence (http://www.iaspei.org/news_items/laquila_IASPEI_press_release_final.pdf /media/vedurstofan/utgafa/hlidarefni/ESC-IASPEI-statement-LAquila-2012-1.pdf

• 3. VI_2014_005

  For the classification of wind conditions, wind direction over the lake is rounded to the nearest 45 degrees. area covered in the model with sparse tundra (41.3% of the model land area) is in fact bare rock or sand plains. The model description of surface type is therefore not a likely cause for the strong wintertime cooling, since replacing at least sparsely vegetated areas in the interior of the island /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 4. Press release on the l'Aquila sentence

  30.10.2012 The International Association of Seismology and Physics of the Earth's Interior, IASPEI, has sent a press release on the l'Aquila sentence in Italy. The European Seismological Commission, ESC, has encouraged its representatives in numerous countries /earthquakes-and-volcanism/articles/nr/2568

• 5. 100 years of seismic observations

  in Reykjavík in 1909. The seismograph was a Mainka instrument and it was sent from Germany under the auspices of the International Seismological Association (ISA). The seismograph measured the horizontal north-south component of the ground motion and the records were sent to Strasbourg for analyzing. In 1913 another seismograph of the same type was installed in Reykjavík that measured east-west /earthquakes-and-volcanism/conferences/jsr-2009/100_years/

• 6. 2013_001_Nawri_et_al

  However, these regions above 1000 mASL are glaciers, and are not relevant for wind energy pro- duction. The highest wintertime wind speeds at 50 mAGL over near-coastal terrain in the western part of the island are reduced from 11 – 12 m s 1 to around 10 m s 1, whereas over intermedi- ate terrain in the interior, wind speed is increased from around 7 m s 1 to around 10 m s 1 (not shown). 24 Figure 6 /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 7. 2010_005_

  Temperature . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 17 4.2 Total Precipitation . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 19 5 Seasonal Differences in Climate Trends 20 6 Conclusions 21 5 List of Figures 1 Mean annual surface air temperature during the 1961–90 control period, differ- ences in degrees between the control period and the 2021–50 reference /media/ces/2010_005_.pdf

• 8. Hare-2011-ParticipatoryModelling

  lcolumn ) 3Participatory Modelling in the Water Sector Copyright © 2011 John Wiley & Sons, Ltd and ERP Environment Env. Pol. Gov. (2011) DOI: 10.1002/eet 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 • participatory modelling purposes, • model type, • stakeholders involved, • timing /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 9. VI_2009_006_tt

  the September 2006 jökulhlaup. . . . . . . . . . . . . . . . . . . . . . . . . . . . . 47 6.1 Discharge of jökulhlaup water at the glacier terminus and out of the subglacial lake during the September 2006 jökulhlaup. . . . . . . . . 50 6.2 Volume of floodwater during the September 2006 jökulhlaup. Water volume in the subglacial lake, volume stored subglacially and cumula- tive volume at the glacier /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 10. VI_2015_006

  depth is determined by placing 50 cm of snow water equivalent (SWE) (or 500 kg m 2 of snow) on top of the permanent snow regions, as defined by the model glacier mask. The “snow on glaciers” runs are used for most of the analysis presented here, whereas the “no snow” runs are used in the last section, to determine the impact of glaciers on the thermodynamic properties of the boundary-layer /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf