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Results:

• 1. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  -corrected SPOT 5 high-resolution geometric (HRG) images with 2.5 m 2.5 m spatial resolution, acquired in the autumn 2003 and (4) airborne polarimetric synthetic aperture radar images observed simultaneously to the 1998 EMISAR images and the EMISAR DEM viewed as a shaded relief image (Magnu´sson et al. 2005b). We estimate the average specific net mass balance (in m yr1 w. eq.) as bn r DV A1  N /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 2. Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication

  are organized by self-identified primary research discipline and gender Primary Research Discipline Number (%) E I S N T F P J Biological Sciences 50 (24%) 26 (52%) 24 (48%) 9 (18%) 41 (82%) 22 (44%) 28 (56%) 7 (14%) 43 (86%) Physical Sciences 106 (51%) 56 (53%) 50 (47%) 20 (19%) 86 (81%) 52 (49%) 54 (51%) 29 (27%) 77 (73%) Social Sciences 53 (25%) 31 (58%) 22 (42%) 8 (15%) 45 (85%) 28 (53%) 25 (47 /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf

• 3. 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

• 4. ces-glacier-scaling-memo2009-01

  ), the total change in glaciated area may be approximated as DSa = 1 g DVa V1 S1 ; (8) in case DVa < 0 or if DVa > 0 and there is sufficient previously ice-covered space to readvance the ice margin (and DSa = 0 in case DVa >= 0 and there is insufficient space to advance the ice margin). The change in average ice thickness is Dha = V1 +DVa S1 +DSa h1 ; (9) TóJ 8 5.12.2009 Memo in case DVa < 0, and Dha =DVa /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 5. vanRoosmalen_etal-2009-WRR_2007WR006760

  is completely saturated and the unsaturated zone no longer active. The net horizontal boundary outflow is the Figure 5. Observed and simulated groundwater heads at locations A and B in Figure 2. W00A15 VAN ROOSMALEN ET AL.: CLIMATE AND LAND USE CHANGE 9 of 18 W00A15 net outflow across the catchment boundary and accounts primarily for groundwater flow to the sea. Drain flow includes drainage from groundwater /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 6. Journal_of_Hydrology_Veijalainen_etal

  -HadCM3-Q0a – A1B HadCM3-A1B 5.44 16.8 9 UKMO-HadCM3-Q0a – B1 HadCM3-B1 3.93 15.8 10 CCSM3 – A2 CCSM3-A2 4.75 14.9 11 CCSM3 – A1B CCSM3-A1B 3.54 12.9 12 CCSM3 – B1 CCSM3-B1 2.72 7.8 13 CNRM-CM3 – A2 CNRM-A2 3.50 15.4 14 CNRM-CM3 – A1B CNRM-A1B 3.16 12.3 15 CNRM-CM3 – B1 CNRM-B1 1.80 7.8 16 ECHAM5/MPI-OM RCA3 A1B RCA3-E-A1B 3.50 20.3 17 ECHAM5/MPI-OM REMO A1B REMO-E-A1B 3.36 12.8 18 UKMO-HadCM3-Q3b /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 7. The weather app

  News The weather app The ever changing /about-imo/news/nr/2812

• 8. The weather app improved

  News The weather app improved The ever /about-imo/news/nr/3224

• 9. 2010_005_

  Surface Air Temperature and Precipitation Trends for Iceland in the 21st Century Nikolai Nawri Halldór Björnsson VÍ 2010-005 Skýrsla Surface Air Temperature and Precipitation Trends for Iceland in the 21st Century VÍ 2010-005 ISSN 1670-8261 Skýrsla +354 522 60 00 +354 522 60 06 vedur@vedur.is Veðurstofa Íslands Bústaðavegur 9 150 Reykjavík Nikolai Nawri, Icelandic Meteorological Office Halldór /media/ces/2010_005_.pdf

• 10. Daniell_etal-2010

  the opportunity to link up with an ongoing initiative in spatial planning (Regionale 2010), which enabled those actors, their plans, measures, and potential funding mechanisms to become part of the Dhuenn process [9; Rasche et al. 2007]. Due to external governmental uncertainty, the described niche became even larger. During the process planning and design phases, administrative structures in North /media/loftslag/Daniell_etal-2010.pdf