65 results were found for z 구미휴게텔㎰《dm080.com』✼구미주점□구미업소□구미타이✗구미안마.

Results:

• 11. Refsgaard_etal-2007-Uncertainty-EMS

  on the quantity at hand (strengths and weaknesses in Box 1. The error propagation equation The error propagation equations for the most common operators are (s is the standard deviation): Addition and Subtraction: z ¼ x þ yþ/ or z ¼ x  y/ sz ¼ ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi s2x  þ  s2y  þ/ r Multiplication by an exact number: z /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 12. 2013_001_Nawri_et_al

  the validity of the ideal gas law, hydrostatic balance, a piecewise linear vertical gradient of air temperature, and neglecting the effects of water vapour. Pressure, p, as a function of height can then be derived through vertical integration of the hydrostatic balance equation, and is given by p(h(x;y);z) = p0 exp g R Z h(x;y)+z 0 dx T (x ) ; (5) where p0 is pressure at mean sea level, T /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

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

  at the operational/local level. A calibrated approach (standardized questionnaires and interviews, expert judgment, and reinterpretation of out- comes by means of relevant literature) was used to com- pare the state of affairs in water management in the selected case-studies. Adaptive and integrated water management Given the expected increase of climate-related extreme events, water governance capabilities /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 14. 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

• 15. VI_2014_001

  frequency distributions for Re- gion 1 derived with index flood model no. 6: bµ(D) = a(AP=Z)b ............................ 39 5 Appendix VI - Empirical and modeled daily flood frequency distributions for Region 2 derived with index flood model no. 3: bµ(D) = a(APm)b ......................... 41 Appendix VII - Instantaneous Index flood models for Region 1. .......................... 43 Appendix VIII /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 16. Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games

  An individual who switches from the (18,2) unequal distribution to the (zi , zi ) egalitarian distribution prefers (18,2) over (zi−1, zi−1) but (zi , zi ) over (18,2). The value zi represents the decision number minus one (as in decision 1, zi = 0) of the first decision in which the agent chooses the egalitarian distribution. This individual is therefore indifferent between the (18,2) unequal /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf

• 17. Refsgaard_2-uncertainty

  - nitrate reduction in underground medium medium large large large Model technical uncertainty - numerical approximation small small medium small - bugs in software medium medium small SUM: Importance Type of uncertainty Error propagation Box 1 Error propagation rules using standard deviation (σ ) Addition and Subtraction: z = x + y + .. or z = x - y - .. ..)()( 22 ++= yxz σσσ /media/loftslag/Refsgaard_2-uncertainty.pdf

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

  Council on Water Resources, Carbondale, IL, 1998). 12. K. E. Schilling, E. Z. Stakhiv, in Global Change and Water Resources Management (Water Resources Update No. 112, Universities Council on Water Resources, Carbondale, IL, 1998). 13. J. R. Stedinger, D. Pei, T. A. Cohn, Water Resour. Res. 21, 665 (1985). 14. Z. W. Kundzewicz, L. Somlyódy, Water Resour. Manage. 11, 407 (1997). 15. P. C. D. Milly, K /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 19. Recent publications

  Oddur Sigurðsson, Óðinn Þórarinsson, Philippe Crochet, Tómas Jóhannesson & Þorsteinn Þorsteinsson (2012). Floods in Iceland. In: Z. W. Kundzewicz (ed), Changes in Flood Risk in Europe. Oxfordshire: IAHS Special Publication 10, 257-276. Hálfdán Ágústsson & Haraldur Ólafsson (2012). The bimodal downslope windstorms at Kvisker. Meteorology and Atmospheric Physics 116(1-2), 27-42, doi:10.1007/s00703 /about-imo/arctic/completed-projects/publications/

• 20. Aurora and the Earth's magnetic field

  by a flux of charged particles from the sun. Increased variations of the field are indicative of increased auroral activity. RH-LRV: Leirvogur Magnetic Observatory Figure 3. Measurements during the past 24 hours from Leirvogur. Three components of the magnetic field are shown; vertical component (Z); horizontal component (H); and the declination (D). The graph is from /weather/articles/nr/2549