An extended period of weak flow across Lake Erie leads to a capped, conditionally unstable lower layer of the atmosphere.
NIRSS detects short periods of MOG IFI around the time of the MOG PIREP. The polarized IHL identifies a large volume of airspace south and east of KCLE as SLW='yes icing', which is the direction of the MOG PIREP. The modified single-pol SLW algorithm identifies a much larger volume of airspace at significantly higher altitudes as SLW='yes icing'.
An extended period of weak flow across Lake Erie leads to a capped, conditionally unstable lower layer of the atmosphere.
NIRSS detects significant periods of MOG IFI around the time of the MOG PIREP. The polarized IHL identifies a volume of airspace west of KCLE as SLW='yes icing', which is the direction of the MOG PIREP. The modified single-pol SLW algorithm identifies a much larger volume of airspace at significantly higher altitudes as SLW='yes icing'.