Albany composite soundings for BLcu cases. a), b) 1100 UTC
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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)

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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.


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