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

Results:

• 41. VI_2015_009

  (2012a, 2012b) and in Crochet & Þórarinsdóttir (2014, 2015), different factors can contribute to the development of a poor index flood model, lead- ing to poor estimates of µ(D) at ungauged catchments. Firstly, the model may be inappropriate to describe the spatial variations of µ(D) in the region under study, even though the region is homogeneous. Secondly, the degree of hydrological similarity /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 42. Water_resources_man_Veijalainen_etal

  power production of the two hydro plants in the outflow river of Lake Pielinen was calculated. Impacts of water levels on recreational use were evaluated by calculating the average annual disad- vantage for recreational use in Euros. The calculations were made using functions of disadvantage for recreational use based on questionnaires and land surveys (Verta et al. 2007). These functions describe /media/ces/Water_resources_man_Veijalainen_etal.pdf

• 43. vonKorff_etal-2010

  /media/loftslag/vonKorff_etal-2010.pdf

• 44. Reykholt-abstracts

  /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 45. VI_2020_008

  the horizontal resolution of limited area NWP models has increased markedly. Given the complex orography of Iceland, high horizontal resolution is needed to describe the terrain. This is especially true of the East- and the Westfjord regions as well as Tröllaskagi in the north. The operational NWP system of IMO is the non-hydrostatic HARMONIE–AROME model, with a horizontal resolution of 2.5 km /media/vedurstofan-utgafa-2020/VI_2020_008.pdf

• 46. 2010_012rs

  /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf

• 47. 2013_001_Nawri_et_al

  rather than from the data directly. This reduces the amount of data that needs to be disseminated to a few parameters, that describe each wind speed distribution. Of the various probability density functions for boundary-layer wind speeds, s, the 2-parameter Weibull distribution, f (s;A;k) = k A s A k 1 exp s A k ; (1) is the one most commonly employed for wind energy studies (Morgan /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 48. VI_2015_007

  catchments. Firstly, the model may be inappropriate to describe the spatial varia- tions of µi(D) in the region under study. Secondly, the degree of hydrological similarity between the target catchment and the homogeneous region is too poor. Thirdly, the index flood model is applied to a catchment whose characteristics are beyond the range of characteristics for which the model was developed. Finally /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

• 49. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  endnotes in Table 2), we have added the dimensions agency, governance, awareness raising and education, risk management, and effectiveness of (international) regulation to the four regime elements that Raadgever et al. (idem) used to describe a management regime in their article. Furthermore, we have developed variables and indicators for the added dimensions and adjusted some of the variables /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 50. Moellenkampetal_etal-2010

  work effectively together? Have there been changes since the co-initiation process? If so, changes on what and why? A more complete description of the evaluation-protocol development and procedures is beyond our scope, but is available in Daniell (2008). For our purposes, we will describe a number of methods of data collection used within the protocols that are relevant to our focus of how project /media/loftslag/Moellenkampetal_etal-2010.pdf