Han, Q., W.B. Rossow, J. Zeng, and R. Welch, 2002: Three different behaviors of
liquid water path of water clouds in aerosol - cloud interactions.
Del Genio, A.D., and A.B. Wolf, 2000: The temperature dependence of
the liquid water path of low clouds in the southern great plains.
Not exact matches
If the craft were to crash on the surface
of a cold moon like Enceladus, the RTGs could easily thaw a
path through tens
of kilometers
of ice, and plop down into the
liquid water ocean beneath, though this might take a long time.
While there are some similarities between the approaches, an important difference is that the slab - ocean approach allows surface and MBL temperatures to adjust to the energetic perturbation: positive energetic forcing
of the surface leads to warming, weakens the inversion, and reduces low - cloud cover and
liquid water path (LWP).
Colors show the
liquid water path (amount
of liquid water in atmospheric columns) simulated with PyCLES.
Czekala, H., S. Crewell, C. Simmer, and A. Thiele, 2001: Discrimination
of cloud and rain
liquid water path by groundbased polarized microwave radiometry.
Han, Q., W.B. Rossow, J. Chou, and R.M. Welch, 1998: Global survey
of the relationships
of cloud albedo and
liquid water path with droplet size using ISCCP.
In the extratropics these are caused by a general increase in cloud fraction in a broad range
of heights, and a strong increase
of cloud
liquid water path in the lower troposphere.
Mudslides which are proximately caused by the overflow
of inland or tidal
waters and are akin to a river or
liquid and flowing mud on the surfaces
of normally dry land areas including your residence, as when earth is carried by a current
of water and deposited along the
path of the current.