39 results were found for WA 0821 7001 0763 (FORTRESS) pintu baja fortress tinggi 240 Oudate Kabupaten Waropen Papua.

Results:

• 21. VI_2009_006_tt

  than can be expected to originate from the cauldrons, three to four times the wa- ter equivalent of the accumulation of snow over the watershed of the cauldrons. It has been estimated that flow from the cauldrons, in addition to the jökulhlaups, could be 2–5 m3 s 1 at maximum (Vatnaskil, 2005). It is possible that part of the sulfate-rich groundwater from the glacier comes from the cauldrons /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 22. Milly_etal-2008-Stationarity-dead-Science

  6University of Washington, Seattle, WA 98195, USA. 7NOAA Geophysical Fluid Dynamics Laboratory, Princeton, NJ 08540, USA. *Author for correspondence. E-mail: cmilly@usgs.gov. An uncertain future challenges water planners. Published by AAAS on July 12, 201 1 www.sciencemag.or g Downloaded from 1 FEBRUARY 2008 VOL 319 SCIENCE www.sciencemag.org574 POLICYFORUM combined with opera- tions /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 23. New article on glacier changes in

  cubic kilometers of water), or a total of 540 ± 130 Gt. This corresponds to 16 ± 4% of the volume of the glaciers around 1890. About half of this mass was lost from 1994 to 2019 or 240 ± 20 Gt, which is about 9.6 ± 0.8 Gt / year on average during that period. Vatnajökull has thinned by 45 m on average in the period 1890–2019, Langjökull by 66 m and Hofsjökull by 56 m. This corresponds /about-imo/news/new-article-on-glacier-changes-in-iceland-over-the-past-130-years

• 24. Markarfljót outwash plain and Öræfajökull

  destruction of the road network; In Öræfi, up to 130 lives could be lost and 240–250 people isolated. Chapter VII. Öræfajökull: Evacuation time modelling of areas prone to volcanogenic floods (pdf 2.96 Mb) Pages 141–164 Emmanuel Pagneux Short summary A model of evacuation routes and timing for areas exposed to floods due to eruptive activity of Öræfajökull Volcano is presented. Estimates /hydrology/hazard-risk-assessments/glacial-outburst-floods/markarfljotsaurar-oraefajokull/

• 25. Traffc-maintenance_expenditures

  010 35 826 31 995 14 697 - - 11 565 965 240 1 534 288 1989 99 043 344 975 25 658 417 254 - 6 616 27 444 37 107 11 469 - - - 969 568 1 626 822 1988 89 553 316 711 32 055 370 248 - 4 552 24 027 41 360 9 665 - - - 888 171 1 609 435 1987 95 558 294 548 31 938 366 374 - 7 647 22 013 38 900 11 006 - - - 867 984 1 656 504 1986 70 968 273 286 26 725 324 820 - 7 254 19 103 29 614 11 425 - - - 763 193 1 521 /media/loftslag/Traffc-maintenance_expenditures.pdf

• 26. The weather in Iceland in 2021

  240 hours above the 1991 to 2020 average. The total number of sunshine hours in Akureyri has only once been higher in the record, it was in 2012. The summer was exceptionally sunny in the North and East. July was especially sunny, the sunniest on record in Akureyri. Figure 5: May was particularly sunny in Reykjavík, the sunniest on record, but the summer was gloomy. The year was sunny /about-imo/news/the-weather-in-iceland-in-2021

• 27. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 28. IPPC-2007-ar4_syr

  /media/loftslag/IPPC-2007-ar4_syr.pdf

• 29. VI_2021_008

  /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

• 30. VI_2016_006_rs

  /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf