41 results were found for (q)495455411灰色词排名霸屏蒋...zv86la..imj.

Results:

• 11. 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

• 12. 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

• 13. 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

• 14. VI_2020_008

  Lykilorð: Undirskrift framkvæmdastjóra sviðs: úrkoma, endurkomutími, aftakagreining, þröskuldsaðferðin, 1M5 kort, IDF ferlar precipitation, rainfall, extreme value analysis, return periods, 1M5 map, IDF curves Undirskrift verkefnisstjóra: Yfirfarið af: SG, TóJ, TJ, EBJ Lykilsíða 5 Contents GLOSSARY /media/vedurstofan-utgafa-2020/VI_2020_008.pdf

• 15. raisanen_ruosteenoja_CES_D2.2

  of greenhouse-gas- induced climate change becomes stronger. The sensitivity of the findings to the evolution of greenhouse gas emissions was also studied, by comparing forecasts derived for the SRES B1, A1B and A2 scenarios. However, due to the relatively short time frame considered, this source of uncertainty proved to be smaller than the uncertainties arising from natural climate variability /media/ces/raisanen_ruosteenoja_CES_D2.2.pdf

• 16. VI_2013_008

  J A 0 100 200 30020 0 60 0 100 0 Days since Sept. 1st Q (m ^3 /s) Obs Pred−nearest Pred−weight Method 4 T+2: RMSE−nearest= 69.6 RMSE−weight= 44.5 S O N D J F M A M J J A Figure 7. Observed and predicted daily discharges at vhm 64 for a forecast range (T) of 2 days and water-year 2004–2005, using methods 1 to 4 with rescaling. The 80%, 90% and 95% pre- diction intervals are represented by grey /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 17. Journal_of_Hydrology_Veijalainen_etal

  ) Finland the spring flood peaks are currently by far the largest floods and as they mostly decreased with climate change the magnitude of the annual 2 and 100-year floods decreased. In the north (Fig. 8a) some scenarios still pro- duced large spring floods in 2070–2099. In southern Finland (in the coastal rivers Fig. 8e and in the lake area Fig. 8d) large floods occurred not only in spring but also /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 18. GA_2009_91A_4_Andreassen

  Fokstugu was used, r was 0.882. The differ- ence in r for the two periods is only 0.015 and doesnot indicate a systematic shift in summer tempera-ture due to the change in station location. Mass balance modelThe mass balance model calculates the mass bal- ance, b(z), as the sum of ablation and solid precip-itation: where Q is energy available for melt, Lm is latentheat of melting and Psolid /media/ces/GA_2009_91A_4_Andreassen.pdf

• 19. Water_resources_man_Veijalainen_etal

  Based on a report by Verta et al. (2007) 92. 5 93. 0 93. 5 94. 0 94. 5 95. 0 M A MJ F J J A S O N D Mean 19702000 Min and max 1970–2000, natural rating curve Target water level zone 1 Target water level zone 2 Q=+20% Q=+10% Q= 0% Q=15% Q=30% 92.90 m snow target 1 92.70 m snow target 2 Water level (m ) Month the regulation limits Lake Syväri has target water level zones, which are not legally /media/ces/Water_resources_man_Veijalainen_etal.pdf

• 20. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

  on Climate Change best estimates for the global mean temperature change by the end of the 21st century vary from 1.8 qC to 4.0 qC between the SRES scenarios with the smallest (B1) and the largest (A1FI) greenhouse gas emissions (IPCC 2007). For shorter time horizons, however, the scenario uncertainty is much smaller. On one hand, there is inertia in the socio-economical system /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf