81 results were found for rain gauge.

Results:

• 61. Group3-Road-scenarios

  but the uncertainty range is large. We are looking two cases: worst case (+4 C degrees increase) and best case (1.5 C increase). Increase in prec: more rain in the winter Decrease in the predictability of weather Natural variability ii. Socioeconomics a. Change in traffic volume b. BAU  Ten-year time steps  National main roads  Geographic area: The whole country Fig. 3 /media/loftslag/Group3-Road-scenarios.pdf

• 62. ces-oslo2010_proceedings

  /media/ces/ces-oslo2010_proceedings.pdf

• 63. Information and help

  ? Characteristics The avalanche problem is related to weakening of the snowpack due to the presence of liquid water. Water infiltrates the snowpack due to melt or rain. Expected avalanche types Wet-snow slab avalanchesWet loose snow avalanchesMainly natural avalanches Where? Spatial distribution When sun is the main cause, distribution of the problem is mostly depending on aspect /avalanches/forecast/help

• 64. Journal_of_Hydrology_Veijalainen_etal

  or heavy rain events. Especially in Southern Fin- land mild periods with snowmelt and flooding are not uncommon in winter. In the lake area the largest floods of the central lakes and their outflow rivers are long-lasting volume floods caused by either prolonged heavy rain or melting of deep snowpack or both. (Mustonen, 1986). 334 N. Veijalainen et al. / Journal of Hydrology 391 (2010) 333–350 /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 65. Increased glacial melt due to volcanic ash

  West Iceland, is a direct run off river. Fig. 4 shows the effect of low precipitation on such rivers. During a dry spell in late summer, water discharge was very low. In preceding years, it was also rather low except during the summer of 2005 (red line). The black line (2010) shows that hardly any rain fell on the drainage area last summer. Location A map which shows the location of various rivers /hydrology/articles/nr/2110

• 66. Eyjafjallajokull_status_2010-04-29_IES_IMO

  images. Heading: West and possibly southwest from the eruption site, but probably remaining close to Eyjafjallajökull due to light winds. Colour: Cloud-cover obscured direct observations. Tephra fallout: Light, fine-grained ash-fall reported in the morning during rain at Ásólfsskáli, located 10.5 km south-west of the eruption site. Similar conditions also reported from a farm 12 /media/jar/Eyjafjallajokull_status_2010-04-29_IES_IMO.pdf

• 67. Helle_Katrine_Andersen_(DANVA,_Dk)

  we transport wastewater in a safe manner and discharge only to the environment when properly treated. The varying amounts of rain are utilized in different ways in the local environment.  Already in the year of 2025 we treat water – including increased amounts of rainwater– as a valuable resource in all parts of the water cycle. The utilities contribute continuously to reduce the global /media/loftslag/Helle_Katrine_Andersen_(DANVA,_Dk).pdf

• 68. Displacements in

  for three different types of slides:Landslides can be released where mountainsides become unstable due to melting of permafrost.Landslides due to heavy rain and snowmelt may become more frequent since warmer winters and increased rain intensity may be expected in warmer climate.Landslides and rockslides may become more frequent where glaciers have receded and thinned so that the lateral /about-imo/news/displacements-in-fagraskogarfjall-for-some-time-before-the-landslide-fell

• 69. QA on the eruption in Eyjafjallajökull 2010

  near the volcano. The difference between the weather in the lowland and in the mountains can be considerable. Wind-chill and wetness (rain, snow or blowing snow) are always a potential hazard, as sudden weather changes are more common on higher ground than in the lowland. How do I find information on present weather in Iceland? For the present weather one can view the newest synoptic analysis /earthquakes-and-volcanism/articles/nr/1880

• 70. The weather in Iceland 2010

  in the summer season, only three times before during the 137 years on record. The lowest minimum was measured at Mývatn on December 22, -28.6°C. The absolute maximum in Reykjavík was 21.2°C, on July 17, and the lowest, -10.8°C, on December 22. Precipitation Precipitation gauge with windshield at IMO's grounds in Reykjavík. Photo by Jón Gunnar Egilsson, 15 September 2010. Precipitation The year /about-imo/news/2011/nr/2112