Step 1: Recall gradient wind balance.
In the northern hemisphere, around curved flow:
- For a low-pressure system (cyclone), the velocity is anticlockwise. Forces balance as:
\[
\text{Pressure Gradient Force (PGF) inward} = \text{Coriolis (to right of flow) + Centrifugal (outward)}.
\]
- For a high-pressure system (anticyclone), the velocity is clockwise. Forces balance as:
\[
\text{Pressure Gradient Force (PGF) outward} = \text{Coriolis (to right of flow inward) + Centrifugal (inward)}.
\]
Step 2: Analyze figure (i).
Low pressure center (L). PGF points inward toward the center. Centrifugal force outward. Coriolis to the right of velocity. This is correct for cyclonic gradient wind.
Step 3: Analyze figure (ii).
High pressure (H). But here the balance shown is inconsistent (PGF direction mismatched).
Step 4: Analyze figure (iii).
High pressure (H). PGF outward, centrifugal outward, Coriolis inward balancing them. This is correct for anticyclonic gradient wind in the Northern Hemisphere.
Step 5: Analyze figure (iv).
Low pressure (L), but the force alignment is incorrect (Coriolis drawn opposite to expected).
Final Answer:
\[
\boxed{\text{(i) and (iii) are correct.}}
\]