I live on the western edge of Australia, with the Indian ocean 10 km
to the west, and the vast desert interior of Australia a few hundred
kilometers to the east.
I've been watching dew point temperature refreshed every 10 minutes on
the weather bureau's website, and I'm wondering what happens to a
moist sea breeze when it blows over the interior, and then returns
much drier. It hasn't dropped any rain, but yet it somehow dries.
If it cools below the dew point (even frost point) overnight, would it
not regain that frost/dew when the land warms up? Or would there be a
time lag, so you would get dried masses of air, that have not had the
opportunity to recapture the dew/frost and then later masses carrying
this evaporated precipitation?
Does the desert act as a dessicant at all?
Perhaps some of the dew/frost (is this called precipitation?) is lost
to lower soil profiles?
Just now, we have an easterly wind that appears to be getting
increasingly humid (specific) and I'm guessing that this actual air
has either not gone over much desert, or has not dropped below the dew
point overnight and is merely a returnimg sea breeze with all of
yesterday afternoon's ocean-derived moisture.
Anyone have any opinions on this? jack