The change in atmospheric pressure ($\Delta P$) due to a change in height ($\Delta h$) can be approximated using the formula:
$\Delta P = -\rho \cdot g \cdot \Delta h$
Where:
The negative sign indicates that pressure decreases as height increases.
We are given:
Substitute these values into the formula:
$\Delta P = -(1.0 \text{ kg/m}^3) \times (9.8 \text{ m/s}^2) \times (200 \text{ m})$
Performing the calculation:
$\Delta P = -1960 \text{ kg} \cdot \text{m/s}^2 / \text{m}^2$
$\Delta P = -1960 \text{ Pa}$
To convert Pascals (Pa) to Kilopascals (KPa), divide by 1000:
$\Delta P = \frac{-1960 \text{ Pa}}{1000 \text{ Pa/KPa}} = -1.96 \text{ KPa}$
The closest approximate answer among the options is -1.9 KPa.
As wind in the lower atmosphere moves over the Earth's surface three forces X, Y and Z shown in the diagram operate on the air mass. If these forces are pressure gradient force (P), Frictional force (F) and Coriolis force (C), find the correct match
| 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.