65 results were found for WA 0859 3970 0884 Bengkel Fabrikasi Vertical Garden Minimalis Kulon Progo.

Results:

• 11. Vertical displacement in the Bárðarbunga caldera

  Disclaimer: These graphs are for civil protection use and to inform the public. They are not to be used in scientific publications without permission. Vertical displacement /earthquakes-and-volcanism/gps-measurements/bardarbunga/caldera/

• 12. Vertical displacement in the Bárðarbunga caldera

  Disclaimer: These graphs are for civil protection use and to inform the public. They are not to be used in scientific publications without permission. Vertical displacement /earthquakes-and-volcanism/gps-measurements/bardarbunga/caldera

• 13. Kok_and_Veldkamp_editorial_ES-2011-4160

  and the environment: the importance of recognizing knowledge claims in transdisciplinary arenas. Ecology and Society 16(1): 21. [online] URL: http://www.ecologyandsociety.org/vol16/iss1/ art21/. Cash, D. W., W. Adger, F. Berkes, P. Garden, L. Lebel, P. Olsson, L. Pritchard, and O. Young. 2006. Scale and cross-scale dynamics: governance and information in a multilevel world. Ecology and Society 11(2): 8 /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf

• 14. Uplift signal detected in Askja volcano

  News The image shows the near-vertical deformation in mm for the period 1-21 August. The InSAR image is obtained from two passages of Sentinel-1 /about-imo/news/uplift-signal-detected-in-askja-volcano

• 15. Ash measurements

  and the the backscatter is measured by the radar. The radar has also been successfully used in monitoring eruption plumes, recording reflections from ash particles and water droplets in the plume. The weather radar on Miðnesheiði The image shows the radar backscatter signal recorded at 14:20 hrs on 23 May 2011. Also, the maximum backscatter in the vertical plane is shown, which can be used /about-imo/news/nr/2183

• 16. HARMONIE - numerical weather prediction model 

  about 1 km to a few km. At IMO the horizontal resolution is 2.5 km. At this resolution it is possible to simulate explicitly some processes that are important for clouds and precipitation, e.g. the vertical movement of air parcels which improves simulations of updrafts and vertical velocity and thus enables the model to simulate larger convective clouds and convective precipitation (rain and snow /weather/articles/nr/3232

• 17. Ash measurements

  the radar backscatter signal recorded at 14:20 hrs on 23 May 2011. Also, the maximum backscatter in the vertical plane is shown, which can be used in estimating the height of the plume. At this time, the plume reached heights of 8 - 12 km. During the 2010 Eyjafjallajökull eruption, the weather radar proved to be a very useful tool, but the great distance to the eruption site (160 km) reduced /about-imo/news/nr/2183/

• 18. Update on Fagradalsfjall

  and vertical components show slight westward and downward movements. The north component is showing slight southward movement. during August we observe a reduction in this trend and it has turned around in the later part of September. A comparable signal is observed on most GNSS stations in Reykjanes signifying a co-eruptive deflation which gradually turns to inflation as the eruption decreases /about-imo/news/update-on-fagradalsfjall

• 19. Ice subsidence above eastern Skaftá cauldron

  This graph shows the ice-surface lowering (subsidence) of the eastern Skaftá ice-cauldron in Vatnajökull ice cap in October 2015. Vertical displacement (m) was monitored by near real time presentation of data from a GPS station, mounted in the middle of the cauldron. The maximum elevation above sea level, top left (hæð), refers to the zero value on the y-axis; while such value top right /hydrology/research/skafta-cauldron/

• 20. Eyjafjallajokull_status_2010-05-11_IES_IMO

  and magnitude less than Ml 2. GPS deformation: Small displacements towards the center of Eyjafjallajökull volcano but irregular oscillations in the vertical component of a station closest to the volcano. Overall assessment: No major changes are seen in the activity, but small variation can still be expected. The ash plume increased slightly in the afternoon. Presently there are no indications /media/jar/Eyjafjallajokull_status_2010-05-11_IES_IMO.pdf