69 results were found for WA 0821 7001 0763 (MEVVAH) Wall Panel Marmer Pp. Terselatan Kabupaten Maluku Barat Daya Maluku.

Results:

• 41. Publications

  - gróðurhúsaáhrif. Lifandi vísindi, pp. 52-54. Snorrason, Á. (2002). Veður, vatn og orka. Presented at the Ársfundur Orkustofnunar 2003, Reykjavík, Mar 20. 31-39. [Extended abstract] Snorrason, Á. (2002). Veðurfar, vatn og orka. Presentation, Aðalfundur Jöklarannsóknafélags Íslands. Norræna húsið, Reykjavík, Iceland. Feb 26. [Presentation] Snorrason, Á. (2004). The International Hydrological /climatology/research/ce/publications/

• 42. 2010_005_

  for Iceland were made. The CE project used an ensemble of six GCMs and RCMs from the PRUDENCE project for four different emissions scenarios (B1, B2, A2, and A1FI) developed by the Intergovernmental Panel on Climate Change (IPCC). The GCMs used by the CE project showed more warming during winter than summer. During winter, the median projected warming from 1961–90 to 2070–99 ranged from 3–6 K, and from 2 /media/ces/2010_005_.pdf

• 43. 2010_016

  the 13 scenarios for annual mean temperature at the meteorological station Hveravellir together with a temperature time-series from Stykkishólmur, western Iceland, that extends back to the early half of the 19th century. The left panel shows that, with the exception of the scenario based on the CSIRO_MK35 GCM model, the scenarios exhibit apparently random interannual to decadal variations /media/ces/2010_016.pdf

• 44. VI_2017_009

  /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 45. Hare-2011-ParticipatoryModelling

  stage )Suppor t an d ski lls n ee de d Har e et a l. (2003 ) X X An aly se lin ks be tw ee n participator y structur e an d proces s implementatio n Ba rr et ea u et a l. (2010 ) X X X Pr o vid e cle ar de sc rip tio n o fproces s (m an ag e ex pe ct at io n s); monitorin g an d evaluatio n Bot s an d va n Daale n (2008 ) X X X X X Su pp o rt pr o ce ss de sig n Ad ap te d fra m ew o rk u se d in th /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 46. Keskitalo_et_al-MLG_and_adaptation_FINAL

  /media/loftslag/Keskitalo_et_al-MLG_and_adaptation_FINAL.pdf

• 47. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  of the decision support tool, BNs created space for an open and non-deterministic dialogue with stakeholders. However, getting stakeholders, citizens and even experts to under- stand and accept the idea behind BNs used for decision making proved to be demanding. BNs are difficult to understand for non-experts and thus requires time and training. Data manipulation is possible and BNs requires a panel /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 48. VI_2021_008

  /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

• 49. Landslides

  increase Landslides also occur at central volcanoes without any volcanic trigger. An example of this is the rockslide in Askja in 2014 where long term subsidence of a caldera wall, formed in volcanic activity in 1875, caused the slope instability. The slide is considered to be one of the biggest rock slides event in Iceland during historical times. More about this landslide in Icelandic can /volcanoes/volcanic-hazards/landslides/

• 50. Seismic signal associated with the Askja rockslide

  in the slope of the caldera wall. The peak in tremor is subsequently caused by the debris fall into the lake. The following flood wave in the lake migrated several times back and forth, causing continuing but decreasing tremor that was seen during the next twenty minutes after the rockslide. There is no evidence for a strong steam explosion in the earthquake data. However it can not be ruled out /earthquakes-and-volcanism/articles/nr/2921