62 results were found for 婷婷丁香玉月（推荐k3t6典CC）up.

Results:

• 31. Eyjafjallajokull_status_2010-05-26_IES_IMO

  : Similar as yesterday, estimated through a webcamera. But in the afternoon the visibility has been very poor caused by ash that has been blown up around the volcano. Because of this, the visibility in Vestmannaeyjar was 1 km and 2 km in Vatnsskarðshólar and the volcano could not be seen on the webcameras in the afternoon. Seismic tremor: Volcanic tremor is still more than before /media/jar/Eyjafjallajokull_status_2010-05-26_IES_IMO.pdf

• 32. Eyjafjallajokull_status_2010-05-28_IES_IMO

  Noises: No reports. Meltwater: Low discharge from Gígjökull. Conditions at eruption site: IES expedition to the summit of Eyjafjallajökull yesterday. Tephra thickness in and around the eastern half of the crates was measured. Tephra up to 40 m thick closes to the craters. Intense steam rises up from the craters, with occasional small ashy explosions. Noise of intense boiling /media/jar/Eyjafjallajokull_status_2010-05-28_IES_IMO.pdf

• 33. Supporting structures stopped most of an avalanche

  snow has piled up against the rows. 1 2 fyrri næsta Supporting structures stopped most of an avalanche Avalanche above the health care centre /about-imo/news/nr/2476/

• 34. Supporting structures stopped most of an avalanche

  has piled up against the rows. 1 2 fyrri næsta Supporting structures stopped most of an avalanche Avalanche above the health care centre of a town /avalanches/articles/nr/2475/

• 35. Eyjafjallajokull_status-leidr_2010-05-05_IES_IMO

  measurements, MODIS satellite image; reports from people via phone and the IMO web site, information from the Icelandic Coast Guard flight yesterday. Eruption plume: Height (a.s.l.): Plume at 5.5-6.5 km height according to IMO's weather radar; reached up to 7.2 km 40 SA of eruption site at 17:45 and 8 km height just SE of eruption site at 16:55. Information from ISAVIA: 18-20,000 ft at 14:50 /media/jar/Eyjafjallajokull_status-leidr_2010-05-05_IES_IMO.pdf

• 36. Further information regarding gas pollution

  rather than towards you.In calm/light wind (<5 m/s) gas can accumulate in the valleys, then circulation is controlled by the landscape and gas can exceed danger levels far up the slopes, all around the eruption site. In such cases, spectators need to move up to higher ground levels such as mountains and ridges and not stay on the slopes just above the eruption. Choose a walking route according /volcanoes/fagradalsfjall-eruption/volcanic-gases/

• 37. Rolf_Johnsen_(Region_Midt,_Dk)

  distribution, less rainfall in summer and more in winter. The precipitation pattern is expected to have a more dynamic cycle, with longer droughts and more intense rainfalls. As a result, groundwater models predict increases in groundwater levels of up to 2 metres in some areas (Van Roosmalen et al). Sea level will also rise. The precise increase is uncertain but models show increases of up /media/loftslag/Rolf_Johnsen_(Region_Midt,_Dk).pdf

• 38. Supporting structures stopped most of an avalanche

  the mountainside (see fig. 1). An avalanche slab was released inbetween the rows of supporting structures. The snow was mostly stopped by the structures and piled up against them (see fig. 2) but part of the snow jumped over the rows. A slab was also released below the lowermost row. The avalanche stopped near the foot of the slope to the west of the structures but before it reached the bottom of the slope /about-imo/news/nr/2476

• 39. Supporting structures stopped most of an avalanche

  near the mountainside (see fig. 1). An avalanche slab was released inbetween the rows of supporting structures. The snow was mostly stopped by the structures and piled up against them (see fig. 2) but part of the snow jumped over the rows. A slab was also released below the lowermost row. The avalanche stopped near the foot of the slope to the west of the structures but before it reached the bottom /avalanches/articles/nr/2475

• 40. Gode_Jenny_CES_2010

  the results from the CES project? – Relevance – Communication – Improvements Stakeholder Relevance of the CES Project Jenny Gode, 31 May 2010 Dialogue meetings square4 3 meetings with stakeholder = "the dialogue group" – Different positions: from R&D, heat production, back up responsibility and up to strategic level square4 Discussions with other stakeholder within Risk Assessment task – Different /media/ces/Gode_Jenny_CES_2010.pdf