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Results:

• 61. Group-1_Scenarios-for-AWM

  t / c o s t ratio H i g h L o w S c enar i o 1 S c ena r io 2 Present time 20302020 Socio E c onomic D e v elopme n t Figure 1. Scenario building for AWM in Horsens Fjord To estimate of the adaptation strategy (Table 2) we will use back-casting approach. The assessments of the productivity of this approach are based on main big strategies which need to have an attention. One of them /media/loftslag/Group-1_Scenarios-for-AWM.pdf

• 62. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

  & 4 Y u a n g Z h e n g D e n m a r k F o r e s t r y & L a n d s c a p e 2 1 0 A t h a n a s i o s V o t s i s F i n l a n d U r b a n & r e g i o n a l p l a n n i n g 3 3 2 E i v i n d J u n k e r N o r w a y L a w 4 3 3 M i c h a e l L a i h o F i n l a n d E u r o p e a n s t u d i e s 5 2 0 H e c to r G u i n e a B a r r i e n to s S w e d e n N a t u r a l r e s o u /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 63. VI_2014_005

  in an overall cold bias, compared with station measurements. To test, whether this is due to the HARMONIE model core or the external surface scheme, biases of 2-m temperature from SURFEX are com- pared with biases of temperature projected from the lowest two model levels to 2 mAGL. It is found that the negative temperature biases are due to shallow inversion layers near the ground, which are introduced /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

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

  ). Locations of the weather sta- tions, used to reconstruct the temperature and precipitation records, are shown with letters: Reykjavík (R), Fagurhólmýri (F), Hæll (H), Stykkishólmur (S), Teigarhorn (T), Vestamannaeyjar (V), Akureyri (A) and Hólar in Hornafjörður (HH). (B) The surface topography of Vatnajökull ice cap. Dots show the sites of mass balance and veloc- ity measurements, blue dots show /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 65. VI2010-006_web

  /media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf

• 66. Publications

  Radic, V., Roald, L. A., Rosberg, J., Rogozova, S., Sigurðsson, O., Suomalainen, M., Thorsteinsson, T., Vehviläinen, B., & Veijalainen, N. (2007). Impacts of climate change on river runoff, glaciers and hydropower in the Nordic area. Joint final report from the CE Hydrological Models and Snow and Ice Groups. Reykjavík: Climate and Energy [Report (high resolution 15 MB)] [Report (low resolution 4 MB /climatology/research/ce/publications/

• 67. Kok_1-scenarios-lecture-1

  : to use or not to use? *O'Neill, R. V., and A. W. King. 1998, Homage to St. Michael; or, why are there so many books on scale?: Pages 3–15 in D. L. Peterson and V. T. Parker (editors). Ecological scale: theory and applications. Columbia University Press, New York. • Robert O’Neill questions the unifying capabilities* • Aspects of the land use system have different scale properties • To use /media/loftslag/Kok_1-scenarios-lecture-1.pdf

• 68. VI_2015_005

  This is also the case with cyclones in all three sectors. Cyclones in the eastern or western sector are also strongly affected by the presence of central cyclones. In both sectors, cyclones tend to move east, unless there are cyclones in the neighbouring sector, in which case pressure tendencies are reversed. 21 Figure 10. Composite mean temporal MSLP tendencies, for different MSLP modes. Com- posite mean /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 69. Recent publications

  61, 1-18. Oddur Sigurðsson (2011). Iceland glaciers. Í: V. P. Singh, P. Singh & U. K. Haritashya (ritstj.). Encyclopedia of Snow, Ice and Glaciers. Springer, Dordrecht, s. 630-636. Árni Snorrason, Jórunn Harðardóttir & Þorsteinn Þorsteinsson (2011). Climate and Energy Systems – Project Structure. In: Þorsteinn Þorsteinsson & Halldór Björnsson (eds.), Climate Change and Energy Systems. Impacts /about-imo/arctic/completed-projects/publications/

• 70. Dyrrdal_Anita_CES_2010

  • Analyse future snow scenarios Introduction Data & Methods Results 0 50 100 150 200 250 300 350 400 450 0-100 100- 200 200- 300 300- 400 400- 500 500- 600 600- 700 700- 800 800- 900 900- 1000 1000- 1100 1100- 1200 1200- 1300 1300- 1400 1400- 1500 1500- 1600 1600- 1700 1700- 1800 1800- 1900 1900- 2000 2000- 2100 2100- 2200 Høyde (m o.h.) A n t a l l v æ r s t a s j o n e r Elevation of met.no /media/ces/Dyrrdal_Anita_CES_2010.pdf