
\begin{tabular}{|c|c|}
\hline Q. 157 & \begin{tabular}{l}
The variation in geostrophic winds with height, in particular, at the atmospheric \\
boundary layer, considering the variation in pressure gradient as a function of \\
height, is referred to as
\end{tabular} \\
\hline
- & Isallobaric winds \\
\hline - & Gradient winds \\
\hline - & Thermal winds \\
\hline - & Cyclostrophic winds \\
\hline
\end{tabular}