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
lidar surveys
Joaquín Muñoz-Cobo Belart, Eyjólfur Magnússon and Finnur Pálsson .......................... 11
Mass balance analysis of Drangajökull ice cap from historical photogrammetry and lidar
Beata Csatho, Thorsten Markus and Thomas Neumann ................................................... 12
The ICESat-2 mission: design, applications and pre-launch performance assessments
/media/vatnafar/joklar/Reykholt-abstracts.pdf
(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
level coursed by tides is small with a range of less than 0.5 m.
Figur 1. Horsens Fjord catchment. WFD main catchment area is 794 km2
NONAM Summerschool Copenhagen 22-26 August 2011 2
Physical features and ecosystem
The fjord landscape is formed by glacial deposits. The average depth is 5 meters and the residence time
of water in the fjord is about 20 days. As to tidal variations
/media/loftslag/Horsens_case.pdf
in sea surface level in the North Sea/Baltic Sea system
whereas changes in sea surface level coursed by tides is small with a range of less than 0.5 m.
Figur 1. Horsens Fjord catchment. WFD main catchment area is 794 km2
NONAM Risk Assessment and Stakeholder Investment. Multidisciplinary Workshop in Reykjavík 26 – 27 August 2010 2
Physical features and ecosystem
The fjord landscape
/media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf
in sea surface level in the North Sea/Baltic Sea system
whereas changes in sea surface level coursed by tides is small with a range of less than 0.5 m.
Figur 1. Horsens Fjord catchment. WFD main catchment area is 794 km2
NONAM Risk Assessment and Stakeholder Investment. Multidisciplinary Workshop in Reykjavík 26 – 27 August 2010 2
Physical features and ecosystem
The fjord landscape
/media/loftslag/Case_A___Horsens_Fjord.pdf
NONAM PhD course – Adaptive management in relation to climate change – Copenhagen 21-26/8/2011
……………………………………………………………………………………………………………………………………………………………………
1
Outline for the case Road maintenance in a changing climate
Introduction
Roads and transport systems are vulnerable to climate change impacts (VTT 2011; Koetse and
Rietveld, 2009; Regmi & Hanaoka, 2011; Road ERA-net 2009 & 2010
/media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf
NONAM
Nordic Network on Adaptive Management in relation to climate change
Risk Assessment and Stakeholder
Involvement
Multidisciplinary Workshop in Reykjavík
26 - 27 August 2010
Final report
NONAM Workshop Reykjavik 26 & 27 August 2010 – Summary
2
Contents
Introduction
/media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf