Adiabatic wind. the normal airflow over the rocky mountains is west to east. the air loses much of its moisture content and is chilled as it climbs the western side of the mountains. when it descends on the eastern side, the increase in pressure toward lower altitudes causes the temperature to increase. the flow, then called a chinook wind, can rapidly raise the air temperature at the base of the mountains. assume that the air pressure p depends on altitude y according to , where p0 = 1.00 atm and a = 1.16 x 10-4 m-1. also assume that the ratio of the molar specific heats is γ = 4/3. a parcel of air with an initial temperature of -5.00°c descends adiabatically from y1 = 4944 m to y2 = 1892 m. what is its temperature at the end of the descent?

the following is queen elizabeth’s purposes:

- to encourage the parliament that the technique of picking successors to the seat based merely on birthright needs to be reviewed.

- (not) to convince the parliament that her kid should not be measured as a likely choice for heir to the english power.

- to persuade the parliament that merely since she has a child does not assure that the kid will be a capable leader.

- to sway the parliament how shattering it could be if they proceeded discourteously concerning her or her child.

96.77 amp

explanation:

rl = 250/100 = 2.5 ohms.

egl = 250 + (100 × 0.1) + 2 = 262 v.

at 700 r.p.m., eg2 = 262 × 700/1000 = 183.4 v.

if ia is the new current, then eg2 - 2 - (ia × 0.1) = 2.5 ia

which means this will give ia = 96.77 amp.