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1. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

1 PhD Workshop preceding Adaptation Research Conference – 27 & 28 August, Helsinki Climate change adaptation - Analysis, Planning and Implementation Programme Venue: Rantapuisto, Ramsinniementie 14, FIN-00980 HELSINKI directions for travel can be found at the conference web site http://www.nordicadaptation2012.net/ Informal start at 26 August On Sunday evening 8pm an informal get /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf
2. VI_2015_006

for the three days considered here, are listed in Table 1. Changes in orbital parameters are mainly significant between the last and the previous two cases, with a drop in noontime solar intensity, defined as the sine of the sun altitude angle, by 14–17%. This difference needs to be taken into account when comparing shortwave radiation fluxes between the different cases. The diurnal cycles of net /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf
3. Machguth_Horst_CES_2010

experiments with different RCM’s • explore RCM biases • apply a different mass balance model data 2 RCM’s • HIRHAM4, Scenario A1B, 25 km, 1950-2100, Greenland • RCAO, Scenario A1B, 50 km, 1960-2100, Pan-Arctic 4 Weather Stations (Ta, Sin) • GC-Net Swiss Camp: 1150 m a.s.l. (1995 – 2006) • GC-Net Crawford: 2020 m a.s.l. (1995 – 2006) • Asiaq Station 437: 300 m a.s.l. (1983 – 2006) • DMI Illulisat /media/ces/Machguth_Horst_CES_2010.pdf
4. GA_2009_91A_4_Andreassen

in southern Norway (Fig.1). The glacier has a total area of 5.4 km2 and rangesin altitude from 1390 to 2090 m a.s.l. The glacierhas been mapped repeatedly, the most recent mapis from 1997. Areas calculated from the 1951 and1997 maps reveal an area reduction of about 0.4km2 in this period (Andreassen 1999). Lengthchange observations reveal a net retreat of about 60 m from 1997 to 2006 (data: NVE; e.g /media/ces/GA_2009_91A_4_Andreassen.pdf
5. Traffc-maintenance_expenditures

047 13 903 11 197 - - - 522 610 1 406 449 1980 42 409 153 761 14 024 212 220 - 5 257 17 816 10 410 9 234 - - - 465 133 1 420 546 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 /media/loftslag/Traffc-maintenance_expenditures.pdf
6. Horsens_case

NONAM Summerschool Copenhagen 22-26 August 2011 1 HORSENS FJORD CASE Hans Jørgen Henriksen, GEUS 1. Background to the case Introducing the catchment Horsens Fjord is a shallow and eutrophic estuary located on the east side of Jutland, Denmark within the WFD catchment area Horsens Fjord (Fig. 1). The surface area of the Fjord is approximately 46 km2 and the mean depth is 2.9 m besides /media/loftslag/Horsens_case.pdf
7. CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction

NONAM Risk Assessment and Stakeholder Investment. Multidisciplinary Workshop in Reykjavík 26 – 27 August 2010 1 HORSENS FJORD CASE Jes Pedersen, Rolf Johnsen and Hans Jørgen Henriksen 1. Background to the case Introducing the catchment Horsens estuary is a shallow and eutrophic estuary located on the east side of Jutland, Denmark within the WFD catchment area Horsens Fjord (Fig. 1 /media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf
8. Case_A___Horsens_Fjord

NONAM Risk Assessment and Stakeholder Investment. Multidisciplinary Workshop in Reykjavík 26 – 27 August 2010 1 HORSENS FJORD CASE Jes Pedersen, Rolf Johnsen and Hans Jørgen Henriksen 1. Background to the case Introducing the catchment Horsens estuary is a shallow and eutrophic estuary located on the east side of Jutland, Denmark within the WFD catchment area Horsens Fjord (Fig. 1 /media/loftslag/Case_A___Horsens_Fjord.pdf
9. vanRoosmalen_etal-2009-WRR_2007WR006760

1998] and RCM output such as incoming and outgoing, short- and long-wave radiation, temperature, water vapor pressure, and wind speed: ETref ¼ 0:408D Rn Gð Þ þ g 900T þ 273 u2 es eað Þ Dþ g 1þ 0:34u2ð Þ ð3Þ where ETref is reference evapotranspiration (mm d1), Rn is net radiation at the crop surface (MJ m2 d1), G is soil heat flux density (MJ m2 d1), T is mean daily air temperature at 2 m /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
10. Instructions on using Atlantic Ocean forecasts

mm to 30 mm every six hours. Light and heavy precipitation is represented by light-green and purple shading, respectively. Atmospheric pressure at the ocean surface is also shown in millibars (1 mb = 1 hPa). The sliding bar below the map is used to change the validity time of the forecast It is possible to change the validity time in many ways: It is possible to click anywhere /weather/articles/nr/1218