Complete the table below. Determine the parcel temperature, parcel dew point temperature and stability at each level.

Height (km), Environmental Temperature (°C), Parcel Temperature (°C), Parcel Dew Point Temperature (°C), Stability
9 -27
8 -20
7 -13
6 -6
5 1
4 8
3 15
2 22
1 29
0 36 36 12

each column is the number for each category

To determine the parcel temperature, parcel dew point temperature, and stability at each level, we need to compare the environmental temperature with the parcel temperature.

1. Parcel Temperature: The parcel temperature represents the temperature of a hypothetical air parcel that rises vertically from the surface to the given height. Initially, the parcel temperature is equal to the surface temperature, given as 36°C at the 0 km level. Remember that the parcel temperature changes when the parcel rises or sinks due to adiabatic processes.

2. Parcel Dew Point Temperature: The parcel dew point temperature represents the temperature at which the air parcel becomes saturated if it is lifted or cooled. Initially, the parcel dew point temperature is equal to the surface dew point temperature, which is given as 12°C at the 0 km level. Similar to the parcel temperature, the parcel dew point temperature changes as the parcel rises or sinks.

3. Stability: Stability indicates whether the air parcel will continue to rise or sink when displaced from its initial level. It can be determined by comparing the environmental temperature with the parcel temperature. If the parcel temperature is greater than the environmental temperature, the parcel is warmer and less dense than its surroundings, resulting in unstable conditions. If the parcel temperature is less than the environmental temperature, the parcel is colder and denser than its surroundings, indicating stable conditions.

Using this information, we can complete the table:

Height (km) | Environmental Temperature (°C) | Parcel Temperature (°C) | Parcel Dew Point Temperature (°C) | Stability
-------------------------------------------------------------------------------------------------------------------------------------------------------
9 | -27 | | |
8 | -20 | | |
7 | -13 | | |
6 | -6 | | |
5 | 1 | | |
4 | 8 | | |
3 | 15 | | |
2 | 22 | | |
1 | 29 | | |
0 | 36 | 36 | 12 |

To complete the table, we need to apply adiabatic lapse rates to calculate the parcel temperature and parcel dew point temperature at each level. However, without further information or given lapse rates, it is not possible to accurately determine these values.