59 results were found for Q 두산베어스경기결과 cddc7.com ◎프로모션번호 B77◎함안 프로토 구매🧛무료황금성게임🩰파워사다리전용사이트∥광주복권방ִ두산베어스경기결과좋아요 advocate/.

Results:

• 21. VI_2016_006_rs

  Such landslides fall from a comparatively high elevation, cause extensive disruption and upheaval of loose materials and soils in their way, and can travel considerable distances uphill against opposing slopes. Secondly, there are medium-sized or large, rapid debris flows that are released from com- paratively high elevations and are confined to gullies as they travel down the mountain- side, similar /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 22. aerodrome_summaries_20140603

  M (171FT ) FRE Q UENCIE S (PE R CENT ) O F OCCU R RENC E O F CONCURREN T WIN D DIRECTIO N (I N 30 0 SEC T ORS ) AN D SPEE D (I N KN O TS ) WITHI N SPECIFIE D RANGE S ANN U A L WIN D WIN D SPEE D (KT) ) DIRECTIO N CAL M 1– 5 6–1 0 11–1 5 16–2 0 21–2 5 26–3 0 31–3 5 36–4 0 41–4 5 46–5 0 >5 0 T O T A L V ARIABL E 0 0 0 0 0 0 0 0 0 0 0 0 0 35-36-0 1 3 2 3 3 2 1 1 0 0 0 0 0 14 02-03-0 4 0 2 4 4 3 1 0 0 /media/vedur/aerodrome_summaries_20140603.pdf

• 23. FMI_-_Disaster_Mitigation

  (Percent) By Year Built Categories Percent of Homes Damaged By Year Built Categories 36 24 26 28 30 32 34 Pre 1980 80-96 97-2002 Post 2002 Percent Damaged All Homes – Damage Per Square Foot All Homes - Damage Per Square Foot 2 2.5 D a m a g e P e r S q . F o o t 0 0.5 1 1.5 < 120 120-129 130-139 140-149 > 149 D a m a g e P e r S q . F o o t Pre 1980 1980-1996 1997-2002 Post 2002 /media/loftslag/FMI_-_Disaster_Mitigation.pdf

• 24. Mid-Latitudes-Agenda1_nov2013EH

  Thursday, 14 November Time Agenda Item 09:00 – 10:30 09:00 – 09:20 09:20 – 09:40 09:40 – 10:00 10:00 – 10:30 Potential Arctic / Mid-Latitude Linkages - East Asia (Chair: Jim Overland) Rapid Arctic Warming in Recent Decades and Its Impact on Climate Change over East Asia - S-J Kim Extreme weather in northern mid-latitudes linked to cryosphere loss - Q Tang A cause of the AO /media/loftslag/Mid-Latitudes-Agenda1_nov2013EH.pdf

• 25. ces-glacier-scaling-memo2009-01

  of melt water from glaciated areas in long integrations for a warming climate. Glacier dynamics This problem can be qualitatively analysed by considering the continuity equation for ice vol- ume, which may be expressed as ¶h ¶t + ¶q ¶x = b or ¶h ¶t +~ ~q = b ; (1) for a one-dimensional ice flow channel or an ice cap that flows in two horizontal dimensions, respectively. h is ice thickness, q or ~q /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 26. 2013_001_Nawri_et_al

  time-series. For wind energy assessments, the main emphasis is on an accurate determination of average wind power density. As discussed in previous sections, average power density is approximately propor- tional to the mean cube of wind speed. Rescaling factors for modelled wind speed time-series, interpolated to station locations, are therefore defined here as 3 q S3o=S3m. Aside from /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 27. 2010_005_

  which are significantly lower com- pared with similar beginning and end years. Consequently, for the 2004–50 period, the average RCM warming rates of 0.29 K per decade over the ocean, and 0.35 K per decade over the land are somewhat larger than for the reduced IPCC ensemble mean. Additionally, the tabulated values of SAT differences between the 1961–90 control period and either the 2021–50 /media/ces/2010_005_.pdf

• 28. Traffc-maintenance_expenditures

  Manage- Basic Purchase Road Road net- Const- Acquisi- Govern- Com- Participati- Value Miscel- Total 2009 ment and road of equip- system work post- ruction tion of ment missi- on of the added laneous cost operating manage- ment develop- poned-, of land grants ons European tax over- level costs ment ment comprehen- build- and com- Regional De- heads 1991- 1991- sive- and ings pensation /media/loftslag/Traffc-maintenance_expenditures.pdf

• 29. VI_2020_008

  a precipitation value from a given location based on values from a regular gridded dataset. ................................................................................................. 28 Figure 7. Scatterplots and Q–Q plots comparing daily precipitation from the ICRA dataset and observations with different extraction methods for station Eskifjörður. .................................. 30 /media/vedurstofan-utgafa-2020/VI_2020_008.pdf

• 30. raisanen_ruosteenoja_CES_D2.2

  in Table 2.1. Some potential limitations of using the CMIP3 ensemble for probabilistic climate change forecasting should be mentioned. First, current GCMs still have a relatively coarse horizontal resolution. Within the CMIP3 ensemble, the grid spacing varies from 1.1 q latitude × 1.1q longitude to 4 q latitude × 5q longitude (for the analysis presented here, all the model results were /media/ces/raisanen_ruosteenoja_CES_D2.2.pdf