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

Results:

• 31. Kok_et_al._TFSC_published_2011

  Exploratory and normative scenario developers both have acknowledged the added value of either type of scenario process. Particularly the backcasting community has attempted to combine backcasting and foresighting approaches. Good examples are Robinson et al. [10], Carlsson-Kanyama et al. [11], and the work of David Banister (e.g. [12]). In this paper we describe an attempt from the community /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

• 32. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

  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 in external forcing. z Natural climate variability, resulting in part from variations in solar and volcanic activity but at least as importantly from the internal dynamics of the climate system /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf

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

  data from two meteorological stations*Vı´k in My´rdalur, close to the ice caps and about 2 km from the coastline and Hveravellir in central Iceland (Fig. 1)*to estimate the mass balance sensitivity to summer and annual temperature variations. Those sta- tions were selected as they include temperature records reaching back to 1979 and describe the different climate conditions south and north /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

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

  be presented in a way which displays the conflicts clearly? My questions to ask others at the Ph.D. workshop would be: how can data best be used in the lay-out of a Ph.D. thesis? I would propose to select some of my empirical research material and describe in which way it relates to my Ph.D. thesis arguments. Then others could give me feedback. 2. Looking at such a wide range of political actors in my /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 35. IPPC-2007-ar4_syr

  summarises the major robust findings and remain- ing key uncertainties in this assessment. A schematic framework representing anthropogenic drivers, impacts of and responses to climate change, and their linkages, is shown in Figure I.1. At the time of the Third Assessment Report (TAR) in 2001, information was mainly available to describe the linkages clockwise, i.e. to derive climatic changes /media/loftslag/IPPC-2007-ar4_syr.pdf

• 36. VI_2022_006_extreme

  and documented in Björnsson et al. (2018) and Crochet et al. (2007). The study, based on the previous research of Jónas Elíasson (Elíasson, 2000; Elíasson et al., 2009) also presented intensity-duration-frequency curves for over 40 locations in Iceland. These curves describe the relationship between rainfall intensity, duration, and return periods, making them useful for flood warnings /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 37. VI_2020_004

  calculate the associated plume height. The need to numerically describe this process is because often the volcanic plume is bent by wind action. Neglecting this aspect would cause an underestimation of the mass flow rate. As a consequence, the way the plume model has been used has been by matching the reported plume height for the different scenarios and identifying those erupting conditions /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 38. VI_2020_005

  of what may happen in the future after adapting the event to modern or future conditions. Statistical models based on the instrumental record do not necessarily include the most drastic events possible since confidence intervals usually describe how well the models fit the data used without considering how well the data represents what may happen. There- fore, information about historical events /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 39. VI_2017_009

  are compared between the reference period and the late-century, a change in the direction of winter winds in the north stands out. This is most prominent in case 2 and only seen slightly in other cases. According to Figure 26, the most prominent winds in Akureyri are SW-NE but in actual fact, the winds there are closer to being SSE-NNW. The wind rose is closer to describe conditions just south /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 40. VI_2009_012

  strike-slip records, when compared to European and North-American events of similar sizes and source depths, on normal and oblique faults. This might point to a reason for why the foreign models fail to describe the PGA of our reference events. Ólafsson’s and Sigurbjörnsson’s model is also the one that fits best, within the one standard deviation region of our model D. Table 1 shows /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf