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70 results were found for 【H-PAY.ORG】全新Twitter(X)账号已验证手机号 bt1a4.


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  • 61. GA_2009_91A_4_Andreassen

  • 62. VI_2020_011_en

    17 Eruptions may also have occurred in 1896 south of Hellisey (Þórarinsson, 1965), possibly close to Geirfuglasker and in 1637 south-west of Heimaey (Jóhannesson, H., 1983). Other eruptions have been dated using radioactive disequilibrium between isotopes including Helgafell (5,900 years BP; 226Ra/230Th; Sigmarsson, 1996), Sæfjall (sometimes called Sæfell; 6,220 years BP; 14C /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf
  • 63. VI_2015_005

  • 64. 2010_016

    the following five parameters were adjusted: (1) Storage coefficient of direct runoff kd; (2) storage coefficient of interflow ki; (3) drainage density d; (4) the fraction of surface runoff from snowmelt; and (5) the recession constant krec for the decreasing saturated hydraulic conductivity with increasing depth. For the groundwater flow, adjusted parameters (6–7) are the hydraulic conductivity in the X /media/ces/2010_016.pdf
  • 65. vanRoosmalen_etal-2009-WRR_2007WR006760

    Impact of climate and land use change on the hydrology of a large-scale agricultural catchment Lieke van Roosmalen,1 Torben O. Sonnenborg,2 and Karsten H. Jensen1 Received 5 December 2007; revised 21 November 2008; accepted 19 January 2009; published 18 March 2009. [1] This paper presents a quantitative comparison of plausible climate and land use change impacts on the hydrology of a large-scale /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
  • 66. Eriksson_Garvill_Nordlund_2006

    asked questions about perceived fairness, effectiveness, expected reduction ARTICLE IN PRESS e (1 is a ’ e m n orde , raised tax on fuel (TAX), and improved public transport (PUB)). X/PUB to be a fair measure?’ t driving distance, do you think other car drivers in your municipality e is implemented?’ t driving distance, do you think you would reduce car use if the measure is X/PUB to affect your /media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf
  • 67. VI_2020_008

    Útreikningarnir eru í 2,5 x 2,5 km neti á 1 klukkustundar fresti fyrir tímabilið september 1979 til desember 2016. Einnig eru notaðar sjálfvirkar úrkomumælingar frá 49 stöðvum sem allar hafa mælt samfellt í yfir 10 ár. Í báðum tilvikum er um daggildi að ræða, þ.e. uppsafnaða úrkomu frá miðnætti til miðnættis. Í næmniathugunum eru mælingar frá 12 stöðvum, svokölluðum kjarnastöðvum, skoðaðar /media/vedurstofan-utgafa-2020/VI_2020_008.pdf
  • 68. CES_D2.4_task1

    distribution of anthropogenic climate changes, largely following Räisänen and Ruokolainen (2008a,b). The main features of this procedure are as follows: x Model simulations of 20th and 21st century climate change are used to develop linear regression equations that relate the local temperature or precipitation climate to a smoothed (11-year running mean) evolution of the global mean /media/ces/CES_D2.4_task1.pdf
  • 69. VI_2022_006_extreme

    of the melt season as retrieved by the third filtering method. 15 4.1.2 Results For each catchment, all the dates retrieved by the last filter were stored in a table. These dates were then plotted together, as shown for four catchments in Figure 7. Results for the other catchments are included in Appendix I (Figures I.1 – 11). On each plot, the x-axis shows the 39 years used for the study /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf
  • 70. IPPC-2007-ar4_syr

    series, of which about 28,000 are from European studies. White areas do not contain sufficient observational climate data to estimate a temperature trend. The 2 x 2 boxes show the total number of data series with significant changes (top row) and the percentage of those consistent with warming (bottom row) for (i) continental regions: North America (NAM), Latin America (LA), Europe (EUR), Africa /media/loftslag/IPPC-2007-ar4_syr.pdf

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