72 results were found for 【菲律宾圣安娜私网正网191-1999-2299】圣noiw安15U7.

Results:

• 51. CES_D2.4_task1

  NO +60:23:18 +11:33:37 147 P 184 HALDEN NO +59:07:21 +11:23:18 8 P 185 SUOLOVUOPMI NO +69:35:17 +23:31:54 377 P 188 GLOMFJORD NO +66:49:00 +13:58:59 39 T 190 KARASJOK NO +69:28:00 +25:30:11 129 TP 191 KJOEREMSGRENDE NO +62:06:00 +09:03:00 626 T 21 192 /media/ces/CES_D2.4_task1.pdf

• 52. VI_Arsskyrsla_2018_vef

  landshlutum. Auk þess er meðalhiti síðustu tíu ára örlítið hærri en meðalhiti tíu áranna á undan. hiti °C vik vik Stöð 2009–2018 1961–1990 1999–2008 Reykjavík 5,4 1,0 0,2 Stykkishólmur 4,8 1,3 0,3 Akureyri 4,4 1,2 0,1 Dalatangi 4,8 1,3 0,3 Meðalhiti og vik síðustu tíu ára í Reykjavík, Stykkishólmi, á Akureyri og Dalatanga. Meðalhiti einstakra ára er í öllum tilfellum vel yfir meðaltali /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf

• 53. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  need inclusion (van der Keur et al. 2008). The complete suite of uncertainties has been referred to as the uncertainty cascade (Hulme and Carter 1999; Katz 2002; Foley 2010). Making climate change adaptation decisions is particularly difficult since they rely on uncertainties related to climate projections as well as to developments in natural systems and sectors that are affected by other /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

• 54. Hare-2011-ParticipatoryModelling

  The full list of examples in order of their appearance in Tables 2 and 3 are: (1) Grampian (Polhill et al., 2010); (2) Hase I (Newig et al., 2008); (3) Wadden Sea (Engelen, 2004); (4) Zürich (Pahl-Wostl and Hare, 2004); (5) Nîmes (Etienne et al., 2008b); (6) Hase II (Newig et al., 2008); (7) Iskar (Phase I) (Daniell, 2008); (8) Moorlands (Hare, 1999); (9) Ebro (Valkering et al., 2009); 1A /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 55. VI_2021_008

  methodology is widely utilized by many automatic earthquake detectors, but instead of having window lengths on the order of minutes, like the ALERT module, they have window durations on the order of seconds. A longer STA window duration will make the module less sensitive to small signals (Trnkoczy, 1999). Additionally, the total duration of the STA and LTA windows may not exceed 24 hours /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

• 56. 2010_012rs

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

• 57. Journal_of_Hydrology_Veijalainen_etal

  ; Jylhä et al., 2008; Räisänen, 2008) and to de- crease snowmelt floods, which are currently the largest floods in most parts of Finland. Significant changes in seasonality of runoff and floods may occur in areas where a large proportion of runoff is from snowmelt (e.g. Lettenmaier et al., 1999; Bates et al., 2008). Finland extends from 70 North with sub-arctic climate to 60 North in the margins /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 58. ces_geus_paakitsoq_full_report

  sheet: Greenland Climate Network 1995–1999, Journal of Geophysical Research, 106(D24), 33,951–33,964. Stendel, M., J. H. Christensen, G. Aðalgeirsdóttir, N. Kliem, and M. Drews (2007), Regional climate change for Greenland and surrounding seas part I: Atmosphere and land surface, in Danish Climate Centre Report, vol. 07-02, Danish Meteorological Institute. Thomsen, H., L.Thorning, and O. Olesen (1989 /media/ces/ces_geus_paakitsoq_full_report.pdf

• 59. VI_2022_006_extreme

  /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 60. VI_2017_009

  with Beaufort number 2 is expected to increase the most in the future and strong winds (Beaufort 4 to 10) to decrease. Wind direction Wind directions in Iceland tend to be controlled by orography but, as CORDEX data from the reference period reveals, SW-NE components are the most common in many areas. The NE winds are often cool and associated with cold weather (Olafsson, 1999). When winds /media/vedurstofan-utgafa-2017/VI_2017_009.pdf