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• 21. Factsheet_Bardarbunga_20141105

  NATIONAL COMMISSIONER OF THE ICELANDIC POLICE DEPARTMENT OF CIVIL PROTECTION AND EMERGENCY MANAGEMENT THE SCIENTIFIC ADVISORY BOARD OF THE ICELANDIC CIVIL PROTECTION Date: 05.11.2014 Time: 09:30 Location: Crisis Coordination Centre, Skogarhlid. Regarding: Volcanic activity in the Bardarbunga system. Attending: Scientists from Icelandic Met Office and the Institute of Earth Sciences /media/jar/Factsheet_Bardarbunga_20141105.pdf

• 22. Bardarbunga-2015_MarchAprMay-events

  and a base from the National Land Survey of Iceland (IS50V lmi.is). Presented by the Volcanology- and Natural Hazards group (ij@hi.is) of the Institute of Earth Sciences, University of Iceland. 3 April 2015 - online sensors for sulphur gas Continuous monitoring of SO2 SO2 sensors are now online at the air quality web of EAI, the Environment Agency of Iceland (see Sjálfvirkir /media/jar/Bardarbunga-2015_MarchAprMay-events.pdf

• 23. 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

• 24. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  to determine a global figure for economic impact (From: EM-DAT 2008). 4 Based on baseline assessments of the case-studies in the NeWater- project (http://www.newater.info). 264 P. Huntjens et al. 123 these case-studies, more specifically in their level of AIWM.5 Therefore, this paper intends to identify differ- ences and similarities in AIWM, to detect general patterns, and to compare measures being /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 25. CES_D2.4_VMGO

  5 ECHO-G, Germany/Korea T30L19/0.5-2.8°×2.8°L20 6 GFDL-CM2.1, USA 2.0°×2.5°L24/0.3-1.0°×1.0° 7 IPSL-CM4, France 3.75°x2.5°L19/2°x1°L31 8 MIROC3.2 (medres), Japan T42L20/0.5-1.4°×1.4°L44 9 MRI-CGCM2.3.2, Japan T42L30/0.5-2.0°×2.5°L23 Modeling output involved to calculate extreme indices includes gridded daily distributions of surface air temperature maxima and minima and daily /media/ces/CES_D2.4_VMGO.pdf

• 26. ice-chart_colour-code-standard

  - this is different from “No Information” which indicates that nothing at all is known about the area. 5) No specific colour is assigned to areas of “No Information”; such areas should be clearly indicated on ice charts - text annotation may be used where appropriate; an assigned colour within the code should not be used to indicate “No Information”. 6) Colour codes do not preclude use of black /media/hafis/frodleikur/ice-chart_colour-code-standard.pdf

• 27. 2013_001_Nawri_et_al

  values. For Part 2, data files describing the local wind statistics on the regular model grid covering Iceland are made available through an online wind atlas (follow the link from http://www.vedur.is/vedur/vedurfar/vindorka/). The files contain estimates of Weibull parameters at each grid point, for twelve wind direction sectors, five heights (10, 25, 50, 100, 200 m above ground level (mAGL /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 28. Mid-Latitudes-Agenda1_nov2013EH

  polarity reversal from winter to summer in 2010 and its relation to extreme hot summer associated with polar jet, summer AO and blocking - Y Tachibana Group Discussion 10:30 – 11:00 Coffee Break 11:00 – 12:00 11:00 – 11:20 11:20 – 11:40 11:40 – 12:00 12:00 – 12:30 Potential Arctic / Mid-Latitude Linkages – Large Scale (Chair: Jim Overland) Large scale linkages between fall /media/loftslag/Mid-Latitudes-Agenda1_nov2013EH.pdf

• 29. Glacier change sessions at this year's Arctic Circle

  ) per year. Barbara Barzycka from the Polish Centre for Polar Studies, University of Katowice, discussed the mass balance of glaciers in Svalbard, where the rate of warming exceeds many other parts of the world. The mean annual temperature in the archipelago has risen by 3–5°C in the period 1971–2018 and the estimated annual mass loss from glaciers in Svalbard during 2006–2015 is 9 GT/year /about-imo/news/glacier-change-sessions-at-this-year-s-arctic-circle-assembly

• 30. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  measures for water related sectors in Denmark The key uncertainties related to climate change adaptation in a Danish context are illustrated by examples from the water-related sectors agriculture, freshwater ecology, water infra- structures in rural areas and urban water infrastructures (Tables 2, 3, 4 and 5). The examples have been selected to illustrate the variety of the climate change /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf