A dynamical meter is a specialized unit of length primarily used in fields like meteorology and oceanography. It is fundamentally linked to the concept of geopotential.
Geopotential ($\Phi$) represents the potential energy per unit mass relative to a reference level. It is influenced by gravity ($g$) and geometric height ($h_{geo}$), often approximated by the formula $\Phi \approx g \times h_{geo}$.
The dynamical height ($h_{dyn}$) is defined based on geopotential, using a standard reference gravity ($g_0$). The definition is $\Phi = g_0 \times h_{dyn}$, which implies $h_{dyn} = \Phi / g_0$. This makes $h_{dyn}$ a measure of height relative to geopotential.
We assess the correctness of each statement:
Based on the analysis, Option 4 provides the most accurate and contextually relevant description of the dynamical meter's relationship with geometric height and geopotential.
| A. | Rainbows | P. | Refraction |
| B. | Mirage | Q. | Refraction and Reflection |
| C. | Corona | R. | Refraction, Reflection, Dispersion in ice crystals |
| D. | Halo | S. | Diffraction |

Air rises from point A to C. At point C it reaches the dew point and begins to descend on the leeward side because it is colder than its surroundings. What will happen to the temperature of the descending air?
Read the following statements about land and sea breeze and choose the CORRECT answer.
I. The land breeze is less extensive both vertically and horizontally than the sea breeze
II. Temperature differences between land and sea are rarely as great at night as in the day time.