-
direction (45° from V-axis), then
adiabats are
concave towards the east north-east (31° from V-axis). If
adiabats and
isotherms are
graphed at regular...
- and have a
slight curve. Dry
adiabats are also
straight and have a 45
degree inclination to the left
while moist adiabats are curved. The main
reason that...
-
Emagram diagram showing variation of dry
adiabats (bold lines) and
moist adiabats (dash lines)
according to
pressure and temperature...
-
coincident with the
adiabat S = 0,
although other isotherms and
adiabats are distinct. As no two
adiabats intersect, no
other adiabat can
intersect the...
-
horizontal (acting as the y-axis). Dry
adiabats are
straight and
solid green but are
tilted while moist adiabats do not have the same
slope throughout...
-
horizontal isobars and
provides for a
large angle between isotherms and dry
adiabats,
similar to that in the tephigram. This made the
diagram useful for analysis...
-
early crust. An
adiabat represents a
change of
temperature with
pressure if no heat was lost
through convection.
Early mantle adiabats show crystallisation...
- efficient,
Carnot cycle, the isoc****s (constant volume) are
replaced by
adiabats (no net heat
transfer because no heat transfer). For the
ideal Stirling...
- has axes of
temperature (T) and
pressure (p). In the emagram, the dry
adiabats make an
angle of
about 45
degrees with the isobars,
isotherms are vertical...
- convection,
leading to a
geothermal gradient that is
determined by the
mantle adiabat,
rather than by the
conductive heat
transfer processes that predominate...
