Final answer:
Higher wind speeds at the 300 mb level occur where height contours, as well as isobars on surface weather maps, are spaced closely together, indicating a steeper pressure gradient and leading to stronger winds.
Step-by-step explanation:
The answer to the question regarding higher wind speeds at the 300 mb constant-pressure level in relation to the spacing of height contours is that they are located where the spacings of height contours are generally close together. This is parallel to the observation on surface weather maps, where wind speeds are higher when the isobars are close together. A smaller distance between isobars or height contours indicates a steeper pressure gradient, which results in stronger winds.