74 results were found for WA 0821 1305 0400 Tempat Pasang Paving Grass Block Taman Cluster Perumahan Johar Baru Jakarta Pusat.

Results:

• 31. norsem_slunga

  This explains the Jamison and Cook observation that the measured stresses were as large as the CFS allowed. Note that the stress observations are from the interiors of the small blocks while the CFS limitations just concern the block boundaries and joints within the blocks. These fracture (CFS) limitations thus strongly affects the interiors of the small blocks. Brown /media/norsem/norsem_slunga.pdf

• 32. VI_2020_008

  eru líkari með þeirri aðferð en með hámark innan tímabilsaðferðarinnar (e. Block Maxima). Ferlar sem sýna samtímis ákefð, tímalengd og tíðni (e. Intensity-duration-frequency curves) eru birtir fyrir hverja stöð, byggðir á úrkomumælingum og útreiknaðri úrkomu. Afurðir verkefnisins eru tvö 1M5 kort, í fyrsta lagi kort byggt á daggildum úrkomu (frá miðnætti til miðnætti) tilsvarandi eldri útgáfu og /media/vedurstofan-utgafa-2020/VI_2020_008.pdf

• 33. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

  cluster (see list below) is dealt with. In the first and second set of parallel sessions the topic clusters are the same. For the first set we have allocated participants according to the information given in the application form and abstract. In the second set it is allowed to switch to another topic set, provided that all topic sets are dealt with. More precise guidelines regarding /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 34. PhD Workshop 2012

  structure, analysis or interpretation of their study). Small clusters of 3 or 4 related dissertation projects will be discussed and reviewed with the aid of experts in parallel sessions. Following acceptance and registration for the Workshop, every PhD student will be allocated a mentor from the pool of experts. Each cluster will receive several assignments for group work. The Workshop will also include 2 /nonam/adaption/phd-workshop-2012/

• 35. norsem_begga

  earthquake locations significantly. Our first step is to test the algorithm on a small subset of 215 earthquakes in year 2001, as reported in the SIL catalog, the earthquakes being located in and around the Geysir region in Southern Iceland. Three small areas were active during the year of 2001, although only one of them was recorded to be active as an earthquake sequence (western cluster; main /media/norsem/norsem_begga.pdf

• 36. norsem_korja

  reactivation type (reverse, normal or strike slip) based solely on their azimuth. The earthquakes in the seismically most active area, close to Skellefteå, Sweden along the western coast of the Gulf of Bothnia and its north-easterly continuation, appear to cluster around the shoreline and along post-glacial faults, which are mostly oriented optimally for reverse or strike slip faulting /media/norsem/norsem_korja.pdf

• 37. 2005EO260001

  Dashed lines encompass the V-shaped zone of tephra deposition. (c) Oblique aerial view from west of the tephra plume at Grímsvötn on 2 November. Note the ashfall from the plume. (Photo by M. J. Roberts.) (d) Weather radar image at 0400 UTC on 2 November. The top portion shows its projection on an EW-vertical plane. The minimum detection height for Grímsvötn is seen at 6 km, and the plume extends /media/jar/myndsafn/2005EO260001.pdf

• 38. Avalanche bulletin - Eyjafjörður (experimental)

  { fill: #BDD7EE; } .status1 .s1, .status2 .s2, .status3 .s3, .status4 .s4, .status5 .s5 { fill: #1F4E78; } .status1 .a1, .status2 .a2, .status3 .a3, .status4 .a4, .status5 .a5 { display: block; } /* Elevation */ .elevation { /* width: 255px; height: 197px; */ width: 70px; height: 54px; } .elev-full .mask { clip-path: url(#full); /*clip-path: inset(0 0 0% round 0px /avalanches/forecast/inner_eyjafjordur

• 39. Avalanche bulletin - Tröllaskagi

  { fill: #BDD7EE; } .status1 .s1, .status2 .s2, .status3 .s3, .status4 .s4, .status5 .s5 { fill: #1F4E78; } .status1 .a1, .status2 .a2, .status3 .a3, .status4 .a4, .status5 .a5 { display: block; } /* Elevation */ .elevation { /* width: 255px; height: 197px; */ width: 70px; height: 54px; } .elev-full .mask { clip-path: url(#full); /*clip-path: inset(0 0 0% round 0px /avalanches/forecast/trollaskagi

• 40. Avalanche bulletin - Eyjafjörður (experimental)

  { fill: #BDD7EE; } .status1 .s1, .status2 .s2, .status3 .s3, .status4 .s4, .status5 .s5 { fill: #1F4E78; } .status1 .a1, .status2 .a2, .status3 .a3, .status4 .a4, .status5 .a5 { display: block; } /* Elevation */ .elevation { /* width: 255px; height: 197px; */ width: 70px; height: 54px; } .elev-full .mask { clip-path: url(#full); /*clip-path: inset(0 0 0% round 0px /avalanches/forecast/inner_eyjafjordur/