37 results were found for 十大正规网博靠谱平台注册官网-澳门皇冠体育官网备用-【✔️输入㊙️bet25.net✔️】-十大正规网博靠谱平台注册官网-356平台注册最新-【✔️访问㊙️700bet.net✔️】-十大正规网博靠谱平台注册官网-十大正规网博靠谱平台注册官网-十大正规网博靠谱平台注册官网-【✔️推荐㊙️360bet.net✔️】.

Results:

• 31. VI_2014_005

  and direction, as well as air temperature, from the IMO operational surface station net- work. Most anemometers are installed at 10 m above ground level (mAGL). However, at some stations, surface winds are measured at different heights, h, varying between 4.0 and 18.3 m. 3This is done using a GRIB-API command on Parameter 141 (snow depth) in the earliest boundary data file: grib_set -f -d 0.0 -w /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 32. Bárðarbunga 2014 - August events

  line shows the number of all measured earthquakes but the red line shows the number of earthquakes above 1.5 in magnitude. During these years, the measuring net has improved and become more sensitive. That is the reason for showing the larger earthquakes separately. 18 August 2014 20:45 - An overview of the first three days Since the onset of the earthquake swarm at Bárðarbunga on Saturday /earthquakes-and-volcanism/articles/nr/3000/

• 33. NONAM_1st_workshop_summary_v3

  /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf

• 34. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  in the data used in making the decision and the factors are interlinked, all of which makes the problem highly complex. The part of the net defined by variables and links is relatively easily communicated to stakeholders (Henriksen et al., 2007b). However the tal Management 88 (2008) 1025–1036 quantitative part, with the conditional probability tables (CPTs), the numbers, is the step where /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 35. VI_2009_006_tt

  Year, month max Qm max Qm Qb Vm Vm Vb (m3 s 1) (m3 s 1) (Gl) (Gl) 1955 09 755 213 1957 05 650 110 1960 09 205 1964 03 885 257 1966 10 1040 230 1970 01 1380 1226 493 394 1972 07 1090 922 407 295 1974 12 1270 1224 306 274 1977 02 1160 1108 320 285 1979 09 1220 1140 346 297 1982 01 1140 1077 384 341 1984 08 1560 1426 411 336 1986 11 1308 1290 247 239 1989 07 1288 1159 354 279 1991 08 1120 928 356 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 36. VI_2022_006_extreme

  that, the detrended timeseries would have had a net difference of zero if the negative values had not been set back to zero. This shows that over the 39 years of data, there was a slight precipitation increase for this grid-point. This trend has been removed, resulting in a detrended, almost flat dataset. 29 Figure 14. Regression lines for hourly precipitation timeseries of grid-point [100, 100] from /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 37. VI_Arsskyrsla_2018_vef

  grundvelli myndatöku með flygildum og leysimælitæki (TLS) hefur verið notað við kortlagningu flóðfara og við mat á útbreiðslu og umfangi hlaupa. Þétt net jarðskjálftamæla, sem staðsettir eru á jökulskerjum eða grafnir í jökul, hefur gefið góða raun við ákvörðun á dýpi jarðskjálfta undir jöklum. Kvikuhreyfingar hafa þannig verið kortlagðar og myndun gosrása staðfest af meiri nákvæmni en áður. Þó /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf