66 results were found for WA 0812 2782 5310 Order Gerobak Pentol Dan Sempol Murah Andong Boyolali.

Results:

• 1. VI_2016_006_rs

  have been released from there (Árni Hjartarson, 2015). A first step in the implementation of mitigation measures for the settlement below Þófi was carried out in 2002, when a 100-m long and 3–4-m deep drainage ditch was dug above the fish factory near the western margin of Þófi in order to drain a part of the shelf into Hæðarlækur (Figure 7). The draining is believed to have been successful /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 2. vanRoosmalen_etal-2009-WRR_2007WR006760

  The hydraulic conduc- tivity of the sand formations is generally high, of the order of 10
  4–10
  3 m/s [Harrar et al., 2003; Sonnenborg et al., 2003]. In general, groundwater flows from east to west. At the water divide to the east the hydraulic head level is about 75 masl, decreasing to sea level at the west coast. The average head gradient is 0.001. The seasonal variation in head values is generally less /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 3. VI_2021_008

  methodology is widely utilized by many automatic earthquake detectors, but instead of having window lengths on the order of minutes, like the ALERT module, they have window durations on the order of seconds. A longer STA window duration will make the module less sensitive to small signals (Trnkoczy, 1999). Additionally, the total duration of the STA and LTA windows may not exceed 24 hours /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

• 4. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  processes in order to be able to compare and evaluate alternative management regimes and to implement and support transition processes if required. This article also addresses the question whether a higher level of AIWM is showing a different response in coping with floods and droughts than case-studies with a lower level of AIWM. This will be done by looking at their adaptation strategies /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 5. norsem_ingi

  ), for the purpose of predicting earthquakes, has been described as the Holy Grail of seismology, i.e. highly desirable goal but with elusive results. Preseismic signals of the order of 10– 20%, reported in the 1960ies and 1970ies, have not been convincingly reproduced. Lower level (0.5– 3.5%) coseismic and postseismic in situ changes have, however, repeatedly been reported. Due to lack of seismicity /media/norsem/norsem_ingi.pdf

• 6. IPPC-2007-ar4_syr

  /media/loftslag/IPPC-2007-ar4_syr.pdf

• 7. VI_2009_006_tt

  The volume of storage in the subglacial flood path, reached a maxi- mum of 35 Gl which corresponds to two-thirds of the total flood volume. The volume of subglacial storage was an order of magnitude larger than could have been melted with the initial heat of the lake water and heat formed by friction in the flow along the flood path. The largest part of the space for subglacial storage /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 8. News

  A GPS station was mounted there on 10th July 2015 in order to monitor displacements at Bárðarbunga in the aftermath of the Holuhraun eruption. Further adjustments and maintainance took place in November 2015 (see photos). News 2023 2022 2021 2020 /about-imo/news/bigimg/3345

• 9. Bárðarbunga earthquakes 3D

  of ten days. An unusual presentation in the sense that the surface location is shown on a topographic map at the bottom, instead of at the top, in order to improve visibility and clarify the connection between location and depth. The gray planes represent depths at 0 km, 5 km and 10 km from the true surface. The colour code of the earthquakes indicates days as counting from 16th August which /earthquakes-and-volcanism/articles/nr/2948

• 10. Asbjorn_Aaheim_(CICERO,_Norway)

  Exploring reasons why the risks of natural hazards seem to be ignored by H. Asbjørn Aaheim, CICERO Researchers give different explanations to why the risks of natural hazards seem to be ignored by individuals, and management strategies are often deemed inappropriate. This presentation combines empirical evidence from various disciplines and theoretical insights in order to identify critical /media/loftslag/Asbjorn_Aaheim_(CICERO,_Norway).pdf