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Albany composite soundings for BLcu cases. a), b) 1100 UTC q (K) and q (g / kg). c), d) as in a) and b) but for 2300 UTC. Frontal composite for BLcu cases. (a) Sea level pressure (hPa) and wind speed and direction. One barb equals 1 m s-1. (b) HF H flux (W m-2) and ORE 2-m temperature
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Albany composite soundings for BLcu cases. a), b) 1100 UTC q (K) and q (g / kg). c), d) as in a) and b) but for 2300 UTC.
Frontal composite for BLcu cases. (a) Sea level pressure (hPa) and wind speed and direction. One barb equals 1 m s-1. (b) HF H flux (W m-2) and ORE 2-m temperature (oC). (c) HF LE flux (W m-2) and ORE specific humidity (g kg-1). AJrepresents the morning and PJ is the evening jump in q (see text for explanation). (d) LCL and cloud ceiling at ORE; ML height is from ALB 0000 UT (1900 LT) sounding.
· ceilometer - LCL · budget method - eddy+ storage Composites of the monthly medians of the daily CO2 fluxes, estimated using two methods: 1. Eddy covariance + storage at 58m, km67 2. very simple budget method: Note: dc/dt filtered using two sequential running means (2 hr, 4 hr)
Monthly means of the diurnal cycle of incoming shortwave radiation. Dash-dot line for Pasture site, magenta line for km67.