80 results were found for 【K528.COM】51查开房记录软件 8d04v.

Results:

• 51. Paper-Olafur-Rognvaldsson_92

  a systematic com- parison of results to observed precipitation has been carried out. Un- dercatchment of solid precipitation is dealt with by looking only at days when precipitation is presumably liquid or by considering the occurrence and non-occurrence of precipitation. Away from non- resolved orography, the long term means (months, years) of observed and simulated precipitation are often /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 52. VI_2022_006_extreme

  77 91 109 Hraunaveita 132 116 136 159 117 140 169 Kvíslaveita 48 42 49 58 42 51 61 Sultartangi 66 57 68 80 58 69 84 Þingvallavatn 96 84 99 117 85 102 123 Þórisvatn 47 41 49 57 42 50 60 Tungnaá 76 67 79 92 67 80 98 Ufsarlón 104 92 108 126 93 112 134 36 Figure 19 – 1M5 maps for catchment Hálslón based on the ICRA dataset without projection (top left), with RCP 2.6 and 10th percentile /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 53. VI_2014_005

  in an overall cold bias, compared with station measurements. To test, whether this is due to the HARMONIE model core or the external surface scheme, biases of 2-m temperature from SURFEX are com- pared with biases of temperature projected from the lowest two model levels to 2 mAGL. It is found that the negative temperature biases are due to shallow inversion layers near the ground, which are introduced /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 54. VI_2013_008

  systematically underestimated. The bias is not as pronounced for the non glacial rivers. Com- bining synoptic-scale and basin-scale predictors (method 3) leads to a substantial improvement compared to the use of MSLP fields alone (method 1). Analogue forecasts become similar or better than persistence, depending on catchment and lead time. Usually, persistence performs better for T=1 day and then method 3 /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 55. VI_2014_006

  the com- plexity of the hydrological processes through modelling, but its application is usually limited to the short-range. Although the results demonstrated a great potential for this method, its success- ful application in real-time will strongly depend on the quality and availability of streamflow observations, which can be poor or simply missing during periods of variable durations, e.g /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 56. Bárðarbunga 2014 - November events

  on the northern side of the volcano's caldera. Hardly any earthquake activity was detected along the dyke intrusion. The largest detected earthquake since yesterday's report registered magnitude 4.5. This earthquake occurred at 01:51 today on the northern side of the caldera, see earthquake maps. Of the 40 caldera earthquakes since 10:00 AM yesterday, five exceeded magnitude 4. Overall, seismicity /earthquakes-and-volcanism/articles/nr/3023

• 57. Bardarbunga-2014_November-events

  earthquakes have been detected within Bárðarbunga. Most of the recorded seismicity occurred on the northern side of the volcano's caldera. Hardly any earthquake activity was detected along the dyke intrusion. The largest detected earthquake since yesterday's report registered magnitude 4.5. This earthquake occurred at 01:51 today on the northern side of the caldera, see earthquake maps. Of the 40 /media/jar/Bardarbunga-2014_November-events.pdf

• 58. Bárðarbunga 2014 - November events

  on the northern side of the volcano's caldera. Hardly any earthquake activity was detected along the dyke intrusion. The largest detected earthquake since yesterday's report registered magnitude 4.5. This earthquake occurred at 01:51 today on the northern side of the caldera, see earthquake maps. Of the 40 caldera earthquakes since 10:00 AM yesterday, five exceeded magnitude 4. Overall, seismicity /earthquakes-and-volcanism/articles/nr/3023/

• 59. Lettenmaier_Dennis_CES_2010pdf

  and watershed scale Statistical downscaling Dynamical downscaling 3) Hydrological and water resources implications -- examples 4) Weak links and the path forward 1) Projected global and regional runoff changes Median runoff sensitivities per degree of global warming, from 68 model pairs – 30-year model average runoff minus 1971-2000 model average (23 models, 3 global emissions scenarios) 51 /media/ces/Lettenmaier_Dennis_CES_2010pdf.pdf

• 60. Bárðarbunga 2015 - January events

  Location map of the eruption site north of Bárðarbunga (enlarge). 14 January 2015 10:00 - from geoscientist on duty Almost 50 earthquakes were observed since yesterday morning in Bárðarbunga. The largest quake was of magnitude 4.6 at 17:51 in the northern caldera rim. Another quake of magnitude 4.6 occurred in the southern caldera rim at 15:00 yesterday. In total, seven quakes were registered /earthquakes-and-volcanism/articles/nr/3071