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SFO APPROACH FOG STUDY 07-09 Noel Keene ZOA CWSU Fremont, CA
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SFO APPROACH FOG STUDY 07-09 Reason for study: – Fog causes significant air traffic impacts at San Francisco International Airport(SFO) – Fog is difficult to forecast Overforecast by models CWSU often forecasts earlier clearing than actual – Scenario for fog likely follows a pattern – Increased lead-time for fog events and better accuracy for total clearing will benefit air traffic operations
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Data Analyzed fall/winter data for 2007/2008 and 2008/2009 Parsed out days where 12Z 500mb height was greater than 5690DM and 12Z SFO-SAC pressure gradient > -1mb and < +1mb – All non-frontal fog events occurred in these conditions – Wanted to evaluate conditions affecting fog other than the typical light winds and high pressure
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Data 67 days met initial criteria – 11 fog events – 56 mornings with no fog Fog event considered to occur when visibility <1SM affected SFO approach zone – Did not use 5/8SM because archived SMB observations do not indicate visibilities <1SM
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Data Evaluated several elements – 12Z OAK 500mb height – Onshore pressure gradient (SFO-SAC) – Offshore gradients (SFO-ACV and SFO-TVL) – 10Z dewpoint at SFO approach zone (SMB) – 12Z OAK 925mb wind direction and speed – Time that visual approaches occurred at SFO Typically SCT or less coverage of clds of below 3500ft Typically visibility > 3sm – Forecaster notes taken day of event
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Findings Clearing time later than expected Some correlation between fog occurrence and: – 10Z SMB Dewpoint – 12Z OAK 925mb wind direction Weaker correlation between fog occurrence and: – 12Z SFO-ACV gradient – 12Z SFO-TVL gradient
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Findings Many variables contribute to fog formation over Bay Area – Therefore…correlations for single variables are low Multiple Linear Regression using both 10Z dewpoint and H9 Wind Direction from 180 yielded higher R values Graphical representation yields some insight into important parameters that contribute to fog formation
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Clearing Time When fog occurred…airport arrival rate never reached optimum(45/60) before 18Z Average clearing time 21:31 Two all-day events where fog transitioned to low ceilings
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Clearing Time Avg
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10Z SMB Dewpoint Correlation Correlation between 10Z SMB Dewpoint and Fog Occurrence at SMB – 0.26 Dewpoint values for fog occurrence – Average…………………..46.8 – Standard Deviation….2.1 Dewpoint values for mornings with no fog – Average…………………..43.4 – Standard Deviation….5.0
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10Z SMB Dewpoint Correlation Avg
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12Z OAK 925mb Wind Direction Subtracted 180 from H9 winds and took absolute value – Larger numbers represent more northerly winds Correlation between H9 wind direction and fog occurrence at SMB – 0.20 H9 wind (FM 180) direction values for fog occurrence – Average…………………..147 – Standard Deviation….35 H9 wind (FM 180) direction values for mornings with no fog – Average…………………..124 – Standard Deviation….45
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12Z OAK 925mb Wind Direction Avg
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Multiple Linear Regression Low P-Value and Significance F – Indicates both variables (dwpt and wind dir) have some effect on outcome (if fog occurs or not) Still fairly low correlation (multiple R) – Indicates that using only dewpoint and wind dir to forecast fog would likely yield poor results…this is fairly obvious
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Northerly Flow SFO APPROACH Northerly flow is only direction where no nearby downsloping will occur Source region of northerly flow is North Bay Valleys – Average lower minimum temperatures – SF Bay can achieve saturation more readily
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Conclusions Preconditions for fog during recent fall/winter seasons at SFO approach have been: – H5 Hgt > 5690DM – SFO-SAC pressure gradient -1mb Northerly flow enhances fog formation – Negative SFO-ACV pressure gradient – Significant northerly component to wind at 925mb High dewpoint temp increases chance for fog formation – Fog did not form when 10Z dewpoint temp < 45F – SF Bay does not cool as readily as inland valleys so higher dewpoint is needed Keying in on secondary elements that aid in fog formation should provide better lead-time for fog events On fog event days…clearing at SFO approach not likely before 20Z
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