54 results were found for 부산진슈얼『텔레그램@uy454』텔레그램@uy454 슈얼광고팀 슈얼광고홍보☎슈얼광고회사㋤슈얼구글 ラ籒 describe.

Results:

• 21. raisanen_ruosteenoja_CES_D2.2

  forcing of the climate system, depend on the magnitude of future anthropogenic emissions of greenhouse gases and other radiatively active substances such as aerosol particles and their precursor gases. z Modelling uncertainty that results from our incomplete understanding, and incomplete capability to describe in climate models, the dynamics of the climate system that determine its response to changes /media/ces/raisanen_ruosteenoja_CES_D2.2.pdf

• 22. NONAM_1st_workshop_summary_v3

  models etc. 4. Which action plans / adaptation scenarios are available and should be developed? The groups should here describe how you arrive at decisions on possible adaptation scenarios to be developed and afterwards analysed. What you want to avoid, what could be achieved (SWOT etc.). 5. Which evaluations of effects of climate change are required? Effects could be technical (flooding /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf

• 23. CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction

  in order to reduce hunting pressure on the disturbance of waterbirds. Hydrological modelling A regional groundwater and surface model is constructed in MIKE SHE / MIKE 11 in order to describe climate change effects on groundwater and surface water systems (Fig. 2 and Fig. 3) Figure 2 Regional flow model for catchment area to Horsens Fjord and Norsminde Fjord. The figure also show major highways /media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf

• 24. Case_A___Horsens_Fjord

  to reduce hunting pressure on the disturbance of waterbirds. Hydrological modelling A regional groundwater and surface model is constructed in MIKE SHE / MIKE 11 in order to describe climate change effects on groundwater and surface water systems (Fig. 2 and Fig. 3) Figure 2 Regional flow model for catchment area to Horsens Fjord and Norsminde Fjord. The figure also show major highways /media/loftslag/Case_A___Horsens_Fjord.pdf

• 25. Horsens_case

  in MIKE SHE / MIKE 11 in order to describe climate change effects on groundwater and surface water systems (Fig. 2 and Fig. 3) Figure 2 Regional flow model for catchment area to Horsens Fjord and Norsminde Fjord. The figure also show major highways, main roads and the topography in the area. NONAM Summerschool Copenhagen 22-26 August 2011 3 Figure 3 Zoom in on Horsens by area. Hansted å /media/loftslag/Horsens_case.pdf

• 26. VI_2009_006_tt

  “ice shelf” is used in this thesis to describe the overlying ice cover of the cauldrons as the weight of the ice covers is mostly supported by floatation although they are fundamentally different from the large ice shelves of Antarctica, Greenland and Canada. 2 Chapter 2 Overview of jökulhlaups A jökulhlaup is a sudden emptying of a water body that is formed by a glacier. The water bodies can /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 27. Adalgeirsdottir-etal-tc-5-961-2011

  A conservative vertical error estimate for the reconstructed 1890 DEM is 15–20 m, 10–15 m for the 1936 DEM, 5–10 m for the 1946 DEM and 5 m for the 1989 DEM. Additional information on glacier extent and glacier varia- tions may be extracted from written historical descriptions of local farmers from the 18th and 19th century. They describe the land use (i.e. grassing of cattle and sheep, use of the for- est /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 28. CES_D2.4_task1

  seasonal (December-February, March-May, June-August and September-November) and annual mean values are studied. In this main report, we will first describe the methods, assumptions and data sets used in the analysis (Section 2 and Appendix). Then, an overview of the results for temperature (Section 3) and precipitation (Section 4) is provided. The set of stations for which detailed tables /media/ces/CES_D2.4_task1.pdf

• 29. GA_2009_91A_4_Andreassen

  and Geography 235 extended. Since then mass balance has been meas-ured at 6–10 stakes, snow depth at 100–150 pointsalong sounding profiles, and snow density at one ortwo locations (Fig. 1). The mass balance at Stor-breen is calculated using the stratigraphic method,i.e. between two successive ‘summer surfaces’(surface minima). Consequently, the measure-ments describe the state of the glacier after /media/ces/GA_2009_91A_4_Andreassen.pdf

• 30. Daniell_etal-2010

  Draft documents were also drawn up in between meetings. More detailed information on the process can be found in Speil et al. (2008) and Moellenkamp et al. [2006]. MAJOR CHALLENGES IN PARTICIPATORY EXERCISES; RESULTS OF THE DHUENN PROCESS To provide insights into the issue of informality and formality of participatory approaches in the context of adaptive management, we describe three major Ecology /media/loftslag/Daniell_etal-2010.pdf