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Results:

• 11. vanRoosmalen_etal-2009-WRR_2007WR006760

  for the scenario simulations are the observed daily precipitation, temperature, and ETref data of the climate grid for Denmark. The same input data are used for the hydrological simulations of the current climate. [20] The correction method for precipitation can be formulated as PD i; jð Þ ¼ DP jð Þ  Pobs i; jð Þ; i ¼ 1; 2; :::::; 31; j ¼ 1; 2; ::::; 12 ð1Þ where PD is the precipitation input /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 12. IPPC-2007-ar4_syr

  and their interactions with sustainable develop- Figure I.1. Schematic framework representing anthropogenic drivers, impacts of and responses to climate change, and their linkages. Schematic framework of anthropogenic climate change drivers, impacts and responses ment. Topic 5 assesses the relationship between adaptation and mitigation on a more conceptual basis and takes a longer-term per- spective. Topic 6 /media/loftslag/IPPC-2007-ar4_syr.pdf

• 13. Eyjafjallajokull_status_2010-05-07_IES_IMO

  recorded at 5-13 km depth, but fewer than yesterday. GPS deformation: Measurements from around Eyjafjallajökull indicate no major net discplaceaments, suggesting a stabilization of the surface deformation since yesterday. Other remarks: Grainsize analysis of samples taken of ash that fell on May 3rd at 64 km distance from the eruption site shows that about 5 % of the ash is smaller /media/jar/Eyjafjallajokull_status_2010-05-07_IES_IMO.pdf

• 14. Traffc-maintenance_expenditures

  Manage- Basic Purchase Road Road net- Const- Acquisi- Govern- Com- Participati- Value Miscel- Total 2009 ment and road of equip- system work post- ruction tion of ment missi- on of the added laneous cost operating manage- ment develop- poned-, of land grants ons European tax over- level costs ment ment comprehen- build- and com- Regional De- heads 1991- 1991- sive- and ings pensation /media/loftslag/Traffc-maintenance_expenditures.pdf

• 15. Reykholt-abstracts

  of the cryosphere Reykholt, Iceland, June 20–21, 2013 4 Sessions Thursday, June 20 09:00‒09:10 ‒ Welcome 09:10‒10:30 ‒ Lidar measurements for glacier inventories and mass balance monitoring 11:00‒12:30 ‒ Process studies - I 13:30‒15:00 ‒ Process studies - II 15:30‒17:30 ‒ Lidar measurements from space, incl. video discussion with input from NASA/USA 18:30‒20:00 ‒ Workshop dinner /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 16. Group5-Stakeholders_involvement

  /EPP 2 Stakeholders analysis 26 August 2011 PM/YZ/EPP 3 Stake h o l d e r s P u b l i c / p r i v at e P o w e r l e v e l (“ n u i s an ce” ca p a c i t y ) O r i e n tat i o n H or s t e n s m uni c ipal i t y ( c o m pe t e n t a u t h ori t y ) P u b l i c S t ron g Go v ernanc e N eighbour mun i c i p ali t y P u b l i c S t ron g Go v ernanc e Poli c y /media/loftslag/Group5-Stakeholders_involvement.pdf

• 17. Adalgeirsdottir-etal-tc-5-961-2011

  (DGPS) equipment in 2001. Continuous profiles, approximately 1 km apart, were measured in the accumulation zone and a dense net- work of point measurements were carried out in the abla- tion zone. Digital Elevation Models (DEMs) of the surface and bedrock were created from these data (Fig. 2; Björns- son and Pálsson, 2004). The estimated errors are at most 1–5 m (bias less than 1 m) for the surface /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 18. Guidelines2-for-rapporteurs

  ). This can be helpful with respect to finding a common structure in presenting as well in session reporting (for which angles mentioned in the opening session statements of the Workshop participants can provide checkpoints).” Session rapporteur allocation M o n d a y 2 9 . 8 Y u a n g Z h e n g A t h a n a s i o s V o t s i s E i v i n d J u n k e r M i c h a e l L a i h o H e c to r /media/loftslag/Guidelines2-for-rapporteurs.pdf

• 19. VI_2014_005

  Evaluation of HARMONIE reanalyses of surface air temperature and wind speed over Iceland Nikolai Nawri VÍ 2014-005 Skýrsla 2 Evaluation of HARMONIE reanalyses of surface air temperature and wind speed over Iceland VÍ 2014- 005 ISSN 1670- 8261 Skýrsla +354 522 60 00 vedur @vedur . is Veður st of a Íslands Búst aðaveg ur 7 – 9 108 Reyk j avík Nik olai Nawr i /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 20. 2010_017

  ............................................................................................................................. 24 7 1 Abstract The WaSiM model is used for hydrological modelling at the Icelandic Meteorological Office. The model application has been improved from former use by: i) improving the representation of groundwater by activating the model’s groundwater module; ii) improving the representation of seasonal changes in the Hamon evapotranspiration /media/ces/2010_017.pdf