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  • 61. VI2010-006_web

    milli byggðarinnar á Akureyri og í Fjörunni um aldamótin. Um 1898 var gerður skipulagsuppdráttur af Torfunefi, neðan Grófargils. Þar efldist byggðin og upp úr aldamótunum og myndaðist þar vísir miðbæ alls kaupstaðarins. Um þetta leyti fór gæta hnignunar í Innbænum og flestum meiriháttar byggingum var nú valinn staður í norðurhluta bæjarins. Húsbrunar settu þar auki mark sitt á byggðina á /media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf
  • 62. Gudmundsson-etal-2011-PR-7282-26519-1-PB

    are currently melting at a fast rate. Over recent decades, annual mass balance field observations on the three largest ice caps in Iceland* Langjo¨kull (ca. 900 km2), Hofsjo¨kull (ca. 890 km2) and Vatnajo¨kull (ca. 8100 km2)*show a declining specific mass balance from about 0 m yr1 w. eq. on average from 1980 to 1994 to 1 to 1.3 m yr1 w. eq. on average after 1995 (Bjo¨rnsson et al. 2002 /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf
  • 63. 2013_001_Nawri_et_al

    and a pressure of 1013.25 hPa. In the case of Iceland, the climate deviates significantly from these standard atmospheric conditions. Additionally, terrain elevation varies considerably across the island. Therefore, seasonal and annual differences in air density from the standard value, as well as spatial variability, need to be taken into account. Approximate air density can be calculated by assuming /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
  • 64. Moellenkampetal_etal-2010

    Acteurs et Usages (UMR G-EAU), Cemagref, 4University of Architecture, Civil Engineering and Geodesy, 5Hornsby Shire Council, 6Lisode, 7UN-Water Decade Programme on Capacity Development (UNW-DPC), United Nations University, 8School of Natural and Rural Systems Management, University of Queensland, 9College of Asia and the Pacific, The Australian National University, 10Marine and Atmospheric Research /media/loftslag/Moellenkampetal_etal-2010.pdf
  • 65. vanRoosmalen_etal-2009-WRR_2007WR006760

    and Irrigationa Scenario Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Current 101 85 59 13 6 4 1 6 39 79 84 97 A2 145 132 73 10 10 7 6 8 4 75 92 123 B2 137 119 75 16 6 6 6 5 21 74 110 141 aValues are in millimeters. 10 of 18 W00A15 VAN ROOSMALEN ET AL.: CLIMATE AND LAND USE CHANGE W00A15 time and larger area where groundwater levels rise above the drain levels. Table 6 shows the mean discharges /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
  • 66. VI_2020_005

    and CNES, n.d.; National Center for Atmospheric Research Staff, 2016; Quante and Colijn, 2016). Now, additional altimeters at different orbits perform slightly less accurate measurements up to 82 N and S (Rhein et al., 2013). These records are used to estimate sea surface changes and calculate global mean sea level, a temporal average sea level averaged over the oceans (Church, Clark, et al., 2013 /media/vedurstofan-utgafa-2020/VI_2020_005.pdf
  • 67. VI_2017_009

    we take the corresponding data from the CMIP5 project. Table 1. All GCMs and RCMs used in this study. If a model is available for any of the domains Arctic-44, EURO-44, or EURO-11, it is marked with a v, but with an x if it is unavailable. Model name Type EURO-11 EURO-44 Arctic-44 CCCma-CanESM2 GCM x v v COSMO-CLM4-8-17 RCM v v x CNRM-CERFACS-CNRM-CM5 GCM v v x IHCEC-EC-Earth GCM v v v /media/vedurstofan-utgafa-2017/VI_2017_009.pdf
  • 68. VI_arsskyrsla2020

    of the infrastructure had taken advantage of rapid technological development without assessing the risk to the security aspects of that same infrastructure. The government has called for concrete actions, mainly for the elec- tric grid, but also for communication and connectivity, transport infrastructure and measures regarding avalanche hazards. The Icelandic Met O?ce (IMO) has actively participated in this gap /media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf
  • 69. Daniell_etal-2010

    and evaluating impacts (see also Swallow et al. 2001, van Ast and Boot 2003). METHODS AND DATA This article is based on empirical data that originated from the analysis of the participatory exercise in the Dhuenn basin. The strong involvement of researchers from two research projects (NeWater[1] and ACER[2]) linked by a joint case study led to the variety of sources available for exploration, including /media/loftslag/Daniell_etal-2010.pdf
  • 70. Kok_JGEC658_2009

    and that paving major roads will lead to deforestation. C3: Conservation units. A large percentage of the Amazon (close to 33%) is classified as some kind of protected area. This includes indigenous reserves, federal parks and national parks. Only about 5% is strictly protected, although it is argued that ‘paper parks’ can also be effective. C4: Forest accessibility. The amount of forest /media/loftslag/Kok_JGEC658_2009.pdf

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