99 results were found for [77AGG. COM]m88 slot slot mod uus slot aerox slot svp88 slot rp555 slot wq5.

Results:

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

  During the conference all of you are requested to act as rapporteur in two or three sessions. A preliminary allocation of rapporteur sessions has been made (see below), while accounting for your expertise in certain areas. Participants can suggest changes in the rapporteur session allocation, on the condition a convincing argumentation is provided as well as a confirmed alternative rapporteur /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 2. 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

• 3. 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/

• 4. 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

• 5. GA_2009_91A_4_Andreassen

  (alb: AWS) MODELLING LONG-TERM SUMMER AND WINTER BALANCES ? The authors 2009 Journal compilation ? 2009 Swedish Society for Anthropology and Geography 241 ed temperatures relative to –20°C to account for de-cay of snow albedo at temperatures below the melt-ing point, following a study by Winther (1993). Wetested both approaches, and chose to use –5°C asthe minimum for the accumulated temperature /media/ces/GA_2009_91A_4_Andreassen.pdf

• 6. CES_D2.4_solar_CMIP3

  the A1B scenario. In the panels for winter and autumn, contour interval is 25 MJ m−2, in those for spring and summer 50 MJ m−2. The colour scale is the same in all panels. Fig. A5. The absolute insolation change under the A2 scenario. 11 Fig. A6. The absolute insolation change under the B1 scenario. 12 (B) TIME SERIES Fig. A7 shows the time series of seasonal changes in incident radiation /media/ces/CES_D2.4_solar_CMIP3.pdf

• 7. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  cia l sy ste m ): th re e m ai n gr ou ps o fthreat s ar e at th e scene : cl im at e, so ci o -e co n o m ic s an d gover nanc e 1: M ai nl y ep ist em ic pl us som e onto logi ca l 2:S cenari o Pa rti ci pa to ry pr oc es s (PP ) imp ortan tt o de al w ith un certaint y Pa rti cip at o ry pr o ce ss (PP )im po rta n tt o de al w ith u n ce rta in ty : Pa rti ci pa to ry go al se tti ng :c o n /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 8. 2010_005_

  Century control runs, as well as 21st Century forecast runs, submitted by various institutions to the Intergovernmental Panel on Climate Change (IPCC) for their Forth 11 Table 1. General circulation and regional climate models that were considered in this study. Model Version Model Name, Institute BCCR BCM 2.0 Bergen Climate Model, Bjerknes Centre for Climate Research, Bergen, Norway CCCMA CGCM 3.1 /media/ces/2010_005_.pdf

• 9. Paper-Olafur-Rognvaldsson_92

  for Meteorological Research, Reykjavík, Iceland 5Bergen School of Meteorology, Geophysical Insitute, University of Bergen, Norway †Corresponding author: or@belgingur.is, Orkugarður, Grensásvegur 9, 108 Reykjavík ABSTRACT Atmospheric flow over Iceland has been simulated for the period Jan- uary 1961 to July 2006, using the mesoscale MM5 model driven by initial and boundary data from the ECMWF. Firstly /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 10. Refsgaard_etal-2007-Uncertainty-EMS

  The advantage of Monte Carlo analysis is its general appli- cability and that it does not impose many assumptions on prob- ability distributions and correlations and that it can be linked to any model code. The key limitation is the large run times for computationally intensive models and the huge amount of outputs that are not always straightforward to analyse. 4.8. Multiple model simulation Multiple model /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf