84 results were found for 【K06.CC】哔哩哔哩账号批发交易1组200个直登 2dv7q.

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• 71. ces_geus_paakitsoq_full_report

  Ice Sheet Surface Mass Balance at Paakitsôq, West Greenland, Derived from Future Scenario Regional Climate Model Data Horst Machguth, Andreas Ahlstrøm, GEUS, Copenhagen 1 Introduction Greenland has a large potential for hydro-power production due to its abundant availability of melt water. In the past GEUS has performed intensive glacio-hydrological investigations at Paakitsôq, West Greenland /media/ces/ces_geus_paakitsoq_full_report.pdf

• 72. Factsheet_Bardarbunga_20141203

  The flow of lava was about 200 cubic meters per second in September but the average flow rate for November is estimated to have been under 100 cubic meters per second. The new lava field is the largest in Iceland since the Laki eruption (1783-1784) and it is probably the third largest lava field on the planet over that period. o Gas: For the first time in 150 years, gas pollution from /media/jar/Factsheet_Bardarbunga_20141203.pdf

• 73. Earthquake swarm by Bárðarbunga volcano

  Earthquake swarm by Bárðarbunga volcano 16.8.2014 15:00 At about 3 a.m. this morning (16 August), an earthquake swarm began by Bárðarbunga volcano in NW Vatnajökull ice cap. Over 200 earthquakes have been recorded. The largest earthquakes have magnitudes of around 3 /about-imo/news/nr/2934

• 74. Floods in the Southeast and East fjords

  Their discharge has grown by a factor of ten within 24 hours. The discharge of Geithellnaá was over 480 m3/s at noon 28th Dec., probably the greastest since 1971. The older maximum was 454 m3/s 31.10.1980. The discharge of Fossá has now exceeded 220 m3/s. The last time it exceeded 200 m3/s was 29.12.2006 but the Fossá river maximum also occurred 31.10.1980, i.e. 395 m3/s. River discharge /about-imo/news/nr/3253

• 75. Gauging stations

  and transmits data to the IMO centre at least once a day. The information mainly concerns water-flow, water-level and ground water, and in some cases other environmental factors are being measured. The network includes about 200 gauging stations. They are to a large extent operated for the Ministry of Industry and the National Energy Authority, or for some of the largest energy firms in the country /hydrology/stations/

• 76. Sea ice in October 2009

  was observed close to the mouth of Önundarfjörður. The Cost Guard went on ice-survey the 6th of October. They observed 14 icebergs west and northwest of Westfjords, and most of them were approximately 200 nm from the cost. The iceberg closest to shore was located 77 nm westnorthwest of Bjarg. In addition to a detailed map of the icebergs location, the Cost Guard issued as well infrared (IR) images /sea-ice/monthly/2009/nr/2332

• 77. Hare-2011-ParticipatoryModelling

  Dispatch: 02.08.11 CE: E E T 5 9 0 No. of Pages: 19 ME: 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 Another possible driving force behind its popularity is changing legislation requiring environmental managers and policy-makers to increase stakeholder participation in their work [e.g /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 78. Paper-Olafur-Rognvaldsson_92

  ). Undercatchment of solid precipitation is dealt with by looking only at days when precipitation is presumably liquid (summer or temperature criteria) or by considering the oc- currence and non-occurrence of precipitation. COMPARISON WITH OBSERVED PRECIPITATION Figure 1 shows the relative error of the simulations, (mm5-obs) / obs, for the summer months June, July and August (JJA). It can be seen /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 79. VI_2019_009

  Comparison between data from automatic weather stations and manual observations Ingibjörg Jóhannesdóttir VÍ 2019-009 Report Comparison between data from automatic weather stations and manual observations VÍ 2019-009 ISSN 1670-8261 Report +354 522 60 00 vedur@vedur.is Icelandic Met Office Bústaðavegur 7–9 IS 105 Reykjavík Ingibjörg Jóhannesdóttir, Icelandic Met Office Contents 1 Inngangur /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 80. 2005EO260001

  The recognition of geophysical precursors to volcanic activity is a primary challenge in volcano monitoring. That challenge was successfully met by scientists at the Icelandic Meteorological Offi ce (IMO) before the 1 November 2004 eruption of Grímsvötn, a subglacial volcano beneath the Vatnajökull ice cap, Iceland (Figure 1). Seismic and geodetic precursors were prop- erly recognized /media/jar/myndsafn/2005EO260001.pdf