The correct answer is (a) H=11000-\(\frac{RT_{11}}{g_0}\)ln(\(\frac{p}{p_{11}}\))
To elaborate: The height of the isothermal lower stratosphere is given by H=11000-\(\frac{RT_{11}}{g_0}\)ln(\(\frac{p}{p_{11}}\)) where,
H=geopotential height
R=characteristic gas constant
T11=temperature at 11km
P11=pressure at 11km
g0=acceleration due to gravity
p=pressure.