31 results were found for WA 0821 7001 0763 (FORTRESS) Pintu Rumah Flat Witihama Flores Timur.

Results:

21. VI_2021_008

/media/vedurstofan-utgafa-2021/VI_2021_008.pdf
22. ces-glacier-scaling-memo2009-01

) and to the power 1.25 for an ice cap (cylindrically symmetrical flow system) on a comparatively flat terrain. For other terrain slopes similar relationships with somewhat lower exponents are expected to hold. Scaling relationships similar to Equation (5), with similar exponents as derived and quoted above, may thus be expected to provide an approximation for ice volume for time-dependent variation /media/ces/ces-glacier-scaling-memo2009-01.pdf
23. Hare-2011-ParticipatoryModelling

ea th , th e m et ho d u se d at th is st ag e fo r th es e st ak eh o ld er typ es is sp ec ied .Sh oul d ther e be tw o o r mor e model sbein g develope d in th e process ,the n th e typ e o fmode lt o whic h th e metho d wa s applie d is show n in parentheses .O T re fe rs to th e co m po si tio n o ft he o rg an iz in g te am . Fo r o rg an iz in g te am in vo lve m en t in di ffe re n t pa rt /media/loftslag/Hare-2011-ParticipatoryModelling.pdf
24. Bárðarbunga 2014 - August events

8-12 km. A few were larger than M3. Few earthquakes were located in the Bárðarbunga caldera today. Hidden intrusion View towards north from the Kverk in Kverkfjöll in June 2004. In the foreground is Kverkjökull, white and flat. Left centrally is the edge of Dyngjujökull, north of which the inrusive dike is migrating. In the background Dyngjufjöll, Kollóttadyngja further /earthquakes-and-volcanism/articles/nr/3000
25. Bardarbunga-2014_August-events

in Kverkfjöll in June 2004. In the foreground is Kverkjökull, white and flat. Left centrally is the edge of Dyngjujökull, north of which the inrusive dike is migrating. In the background Dyngjufjöll, Kollóttadyngja further, then Hrúthálsar and then mountain Herðubreið which stands apart. Photo: Erik Sturkell. 26 August 2014 15:45 - status report Overall assessment from the joint daily status /media/jar/Bardarbunga-2014_August-events.pdf
26. Bárðarbunga 2014 - August events

8-12 km. A few were larger than M3. Few earthquakes were located in the Bárðarbunga caldera today. Hidden intrusion View towards north from the Kverk in Kverkfjöll in June 2004. In the foreground is Kverkjökull, white and flat. Left centrally is the edge of Dyngjujökull, north of which the inrusive dike is migrating. In the background Dyngjufjöll, Kollóttadyngja further /earthquakes-and-volcanism/articles/nr/3000/
27. Gudmundsson-etal-2011-PR-7282-26519-1-PB

and spring, indicating a thick winter snow pack at the highest flat part of the accumulation area of Eyjafjallajo¨kull. Temperature observations at both Hveravellir and Vı´k in My´rdalur are used to examine the mass balance sensitivity to increase in temperatures (Table 4). The temperature rise from the first period 19791984 to 1998 to the later period 19982004 is 1.01.2 8C at Hveravellir in central /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf
28. VI_2022_006_extreme

season never started before late April, while in the years after 1995 it would start early-to-mid April. In the case of Hálslón (Figure 7, bottom left), the regression line is flat, indicating no trend for this period, although for the interval 1996 – 2017, except for 2011, the melting started in late May at the latest, whereas previously it could occur as late as early June. The most surprising /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf
29. VI_2009_012

to 8 broad-band sensors distributed around the country. These include CMG-3T, CMG-40T, CMG-ESP and STS2, with corner frequencies at 0.008 and 0.033 Hz. A large portion of the sites are equipped with short-period Nanometrics RD3 digitizers with a corner frequency around 0.5 Hz and the remaining have CMG-DM24 digitizers, with a flat response. The maximum amplitude of the stations varies between 0.3 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf
30. VI_Arsskyrsla_2018_vef

/media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf