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Results:

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

  Reykjavı´k IS-101, Iceland 2 Centre National de la Recherche Scientifique, Universite´ de Toulouse, Laboratoire d’Etudes en Ge´ophysique et Oce´anographie Spatiale, Universite´ de Toulouse, 14 Avenue Edouard Belin, Toulouse FR-31400, France 3 National Space Institute, Technical University of Denmark, Lyngby DK-2800, Denmark Keywords Remote sensing; glacier mass balance; regional warming /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 2. VI_2015_006

  ....................................................................................... 10 3 September 2012 .................................................................................. 12 3 Radiation fluxes at the surface ....................................................................... 16 4 Heat fluxes at the surface .............................................................................. 21 5 Net energy /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 3. vanRoosmalen_etal-2009-WRR_2007WR006760

  such as irrigation, CO2 effects on transpiration, and land use changes affect the water balance to a lesser extent. Citation: van Roosmalen, L., T. O. Sonnenborg, and K. H. Jensen (2009), Impact of climate and land use change on the hydrology of a large-scale agricultural catchment, Water Resour. Res., 45, W00A15, doi:10.1029/2007WR006760. 1. Introduction [2] The most recent Intergovernmental Panel /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 4. 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

• 5. Journal_of_Hydrology_Veijalainen_etal

  24 July 2010 This manuscript was handled by K. Georgakakos, Editor-in-Chief, with the assistance of Ercan Kahya, Associate Editor Keywords: Climate change Flood Hydrological modelling Flood inundation area Hydraulic modelling Finland s u m m a r y This paper provides a general overview of changes in flooding caused by climate change in Finland for the periods 2010–2039 and 2070–2099. Changes /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 6. ces-glacier-scaling-memo2009-01

  A reduction in the glaciated area at the lowest altitudes is specified as DSa1 = kDSa ; (10) where k is an adjustable parameter, 0 < k < 1. This reduction is carried out by eliminating the ice-cover sequentially, starting with the lowest elevation band or grid cell of the group and continuing upward until the total eliminated ice-covered area is equal to DS1. Some ice may remain in the uppermost /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 7. ces_geus_paakitsoq_full_report

  ) is shown. At the margin the grid boxes of the RCAO RCM are visible. The area between Illulisat and Swiss camp is commonly called Paakitsôq. respectively. The Automatic Weather Stations (AWS) Swiss Camp and Crawford are located on the ice sheet and are operated by the Greenland Climate Network (GC-net) (Steffen and Box, 2001). The locations of the stations are indicated in Fig. 1, further details /media/ces/ces_geus_paakitsoq_full_report.pdf

• 8. 2010_005_

  downscaling results previously obtained by Kaas (1993, 1994), as well as results from four different climate models (with the GFDL CM3 as the primary reference). The study found a warming of 0.3 K per decade until the middle of the 21st Century, with a wintertime warming rate of 0.35 K per decade, and a warming rate of 0.25 K per decade in summer. The study also examined precipitation changes and found /media/ces/2010_005_.pdf

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

  Personality type differences between Ph.D. climate researchers and the general public: implications for effective communication C. Susan Weiler & Jason K. Keller & Christina Olex Received: 27 August 2009 /Accepted: 28 July 2011 / Published online: 2 September 2011 # The Author(s) 2011. This article is published with open access at Springerlink.com Abstract Effectively communicating the complexity /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf

• 10. Perrels-CBA

  operational cost, etc.) and the annual revenues • consider an appropriate discount rate and assess NPV (net present value), IRR (internal rate of return), and net cash flows • rank alternatives by score level • SCBA: social CBA – total benefits -/- total costs for society, in this case benefits and costs often don’t accrue (entirely) to the same organisation due to the public nature of a project /media/loftslag/Perrels-CBA.pdf