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  • 1. Refsgaard_1-Welcome

    – Print yourselves • Case descriptions and tasks/questions • Lecturers’ presentations – Handouts during the week – Pdfs will be uploaded at website afterwards Practicalities • PC login – Internet access • Printing • Lunch • Coffee – tea • Posters Monday afternoon + refreshments • Dinner Tuesday at 19:00 Students • Brief presentation round – now • 2-minutes presentation of research topics /media/loftslag/Refsgaard_1-Welcome.pdf
  • 2. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

    with whom a slot is proposed to be swapped. In the closing session on Friday afternoon another two Workshop participants will be offered the opportunity of presenting a brief summary of key impressions and messages (2 x 5 minutes). This will require some degree of co-ordination among the rapporteurs. The Conference organizers need to know in time (Friday morning at the latest) who will present /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf
  • 3. Kurpniece_Liga_CES_2010

    and corrected data -5 0 5 10 15 1 . 0 1 . 5 2 . 0 2 . 5 3 . 0 3 . 5 Temperature,°C P r e c i p i t a t i o n , m m / d a y Jan Feb Mar Apr May Jun JulAug Sep OctNov Dec Year obs ALUKSNE DMI 1961-1990 ALUKSNE mod DMI 1961-1990 ALUKSNE JanFeb Mar Apr May Jun Jul AugSep Oct Nov Dec Year Jan Feb ar Apr May Jun Jul Aug Sep Nov Dec ear After the correction all 3 climate models agree with observed data /media/ces/Kurpniece_Liga_CES_2010.pdf
  • 4. GA_2009_91A_4_Andreassen

    ) and summer balance (bs) have been carried out at Storbreen since 1949. Here we apply a simple mass balance model to study the climate sensitivity and to reconstruct the mass balance series prior to 1949. The model is calibrated and validated with data from an automatic weather station (AWS) operating in the ablation zone of Storbreen since 2001. Re- gression analysis revealed that bw was best mod /media/ces/GA_2009_91A_4_Andreassen.pdf
  • 5. Burnett_Dougal_CES_2010

    of Sunshine Duration to Solar Irradiation • Method used Suehrcke (2000), based on widely used Angstrom-Prescott equation. – Relates the sunshine fraction to monthly average solar radiation – Lots of lower level calculations required: sun–earth variables, latitude, day hours, solar declination, extra-terrestrial irradiation, sunset hour angle…     = OH HK radiation stialextraterre surface /media/ces/Burnett_Dougal_CES_2010.pdf
  • 6. Shipping forecasts

    - east partN 5-10. MOD NIGHT, E 3-8 TOM.Forecast made: 01.05.2023 04:48. Valid until: 03.05.2023 00:00.East Banks - north partN 8-13, 3-8 EVENING. LGT VRB WND TOM AFTERNOON.Forecast made: 01.05.2023 04:48. Valid until: 03.05.2023 00:00.East Banks - south partN 8-13, 3-8 NIGHT.Forecast made: 01.05.2023 04:48. Valid until: 03.05.2023 00:00.Southeast BanksVRB 5-10, E/SE 5-13 TOM AFTERNOON, STRG /weather/shipping/text/
  • 7. Shipping forecasts

    - east partN 5-10. MOD NIGHT, E 3-8 TOM.Forecast made: 01.05.2023 04:48. Valid until: 03.05.2023 00:00.East Banks - north partN 8-13, 3-8 EVENING. LGT VRB WND TOM AFTERNOON.Forecast made: 01.05.2023 04:48. Valid until: 03.05.2023 00:00.East Banks - south partN 8-13, 3-8 NIGHT.Forecast made: 01.05.2023 04:48. Valid until: 03.05.2023 00:00.Southeast BanksVRB 5-10, E/SE 5-13 TOM AFTERNOON, STRG /weather/shipping/text
  • 8. Dyrrdal_Anita_CES_2010

  • 9. Paper-Olafur-Rognvaldsson_92

    a systematic com- parison of results to observed precipitation has been carried out. Un- dercatchment of solid precipitation is dealt with by looking only at days when precipitation is presumably liquid or by considering the occurrence and non-occurrence of precipitation. Away from non- resolved orography, the long term means (months, years) of observed and simulated precipitation are often /media/ces/Paper-Olafur-Rognvaldsson_92.pdf
  • 10. Refsgaard_etal-2007-Uncertainty-EMS

    the study on the elements that produce most infor- mation of relevance to the problem at hand.  STEP 2 (data and conceptualisation). In this step the mod- eller should gather all the relevant knowledge about the study basin and develop an overview of the processes and their interactions in order to conceptualise how the system should be modelled in sufficient detail to meet the requirements /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

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