lec 14 Flashcards
what is fog
condensation in the lower atmos
what are the types of fog
radiative
valley
advection
upslope
mixing
fog drip
radiative fog
forms via a temp inversion- warm air on top of cool air (commonly from radiative cooling). the cooler air near the surface reaches the dew point while the air above does not
radiatve cooling
the emmision of thermal heat from the surface to cool
valley fog
a form of radiation fog, induced by the presence of hillslopes. the coolaer more dense air flows down slope and settles in a valley
advection fog
when warm moist air flows over a cold surface, causing the air parcel to cool to tis dew point.
most common the the coast
upslope fog
warm air force upwards due to a physical barrirer, cauing cooling to dew point.
common near coastal regions with mountains near by
mixing fog
the mixing of 2 near saturation air parcels at differnet temps
fog drip
when the moisture from fog adheres to leaves and needles and drips off.
high source of fresh water (to be included in the water cycle)
water are the different ways clouds can form
convection
orographic uplift
convergence
frontal systems
divergence
high clouds
7km<
cirro-
wispy due to little water and particle presence
middle clouds
2-7km
alto-
commonly formed during weather chnages
low clouds
<2km
no prefix
puffy clouds
cumulus
layered
stratus