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  • 61. Water_resources_man_Veijalainen_etal

    is characterised by temperature-sensitive snow-dominated seasonality, with snow accumulating during N. Veijalainen (B) · T. Dubrovin · M. Marttunen · B. Vehviläinen Finnish Environment Institute, Helsinki, Finland e-mail: noora.veijalainen@ymparisto.fi Author's personal copy 3438 N. Veijalainen et al. winter and snowmelt during spring. This makes the area especially susceptible to major seasonal /media/ces/Water_resources_man_Veijalainen_etal.pdf
  • 62. 2013_001_Nawri_et_al

    of Iceland (Háskóli Íslands; UI) in the context of Work Package 2 of the project “Im- proved Forecast of Wind, Waves and Icing” (IceWind), funded primarily by the Nordic Top-level Research Initiative (Toppforskningsinitiativet; TFI), including national and private organisations. This report is the fifth in a series of IMO reports produced for IceWind, the others being Nawri et al. (2012d,a,b,c /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
  • 63. Hydropower, Hydrology

    Hydrological Sciences Journal, 53, 100-111. Kriauciuniené, J., Meilutyté-Barauskiené, D., Rimkus, E., Kays, J., Vincevicius, A. (2008). Climate change impact on hydrological processes in Lithuanian Nemunas river basin. Baltica, Vol. 21 (1-2), pp. 1-61. Vilnius. ISSN 3067-3064. Lawrence, D., Haddeland, I. (2010). Uncertainty in hydrological modelling of climate change impacts in four Norwegian /ces/publications/nr/1938
  • 64. Climatological data

    © Veðurstofa Íslands | Bústaðavegi 7- 9 | 105 Reykjavík | Phone 522 6000 | Fax: 522 6001 Recording 902 0600 | SSN 630908-0350 Contact us | Employees | Terms and conditions | Sitemap Other related web sites Icelandic Mobile web /climatology/data/
  • 65. Glossary

    We are hoping to find time to improve this glossary. Only a few items are available. For your relevant search, please click on one of the letters below: A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö A A: Icelandic abbreviation of East (compass direction, easterly, eastern). ANA: Icelandic abbreviation of Eastnorthesast (compass direction). ASA: Icelandic /weather/articles/nr/1208
  • 66. Glossary

    We are hoping to find time to improve this glossary. Only a few items are available. For your relevant search, please click on one of the letters below: A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö A A: Icelandic abbreviation of East (compass direction, easterly, eastern). ANA: Icelandic abbreviation of Eastnorthesast (compass direction). ASA: Icelandic /weather/articles/nr/1208/
  • 67. VI_2020_005

    world we live in is continuously changing and developing. Changes in one field often lead to shifts in others. Since the industrial revolution, human lifestyle has significantly influenced the Earth’s atmospheric composition, which is directly and indirectly an important factor in a deli- cate balance of numerous natural phenomena. Anthropogenic actions have thus caused, or sped up alterations /media/vedurstofan-utgafa-2020/VI_2020_005.pdf
  • 68. VI_2015_005

    water. Since, in this study, the focus is on large-scale storm systems, persisting for at least one day, variability on shorter time-scales (mainly the diurnal cycle and atmospheric tides) is eliminated by calculating averages from the four 6-hourly reanalysis fields of each day (6-hourly precip- 8 Figure 1. Top: Average fields of 500 hPa geopotential height in winter (DJF 1989-90) and summer (JJA /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf
  • 69. Bardarbunga_kafli20140825

    frequency during the last 1100 years is 1 eruption per 50 years on average. Eruptions on the ice covered part of the system have the potential to cause major floods in several rivers flowing southwards and northwards from the Vatnajökull ice cap. _________________________________________________________________________ Central volcano: Bárðarbunga Lat, lon: 68°38´N, 17°31´W Elevation: 2009 /media/jar/Bardarbunga_kafli20140825.pdf
  • 70. Kok_et_al._TFSC_published_2011

    development is well-suited to the challenges posed by the WFD to develop a long-term view by involving stakeholders. In this paper we analyse the process and results of a series of stakeholder workshops to develop scenarios at pan-European level. Specifically, we aim at analysing the method and results of combining a backcasting methodology and exploratory scenario development process. Four /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

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