4 formatting
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I'm having a bit of trouble figuring out a solution to this problem:

There is an isothermal layer of air which has a temperature of $0$ degrees Celsius0 °C extending from the surface to $1$1 km height. A parcel is $0.5$ degrees Celsius0.5 °C is released at the surface in the isothermal layer. How high does the parcel rise before it descends back?

I know what an isothermal layer is and I know that the parcel will rise until it reaches the surrounding air temperature. I am just not sure how or which formula I would use to solve the problem.

I'm having a bit of trouble figuring out a solution to this problem:

There is an isothermal layer of air which has a temperature of $0$ degrees Celsius extending from the surface to $1$ km height. A parcel is $0.5$ degrees Celsius is released at the surface in the isothermal layer. How high does the parcel rise before it descends back?

I know what an isothermal layer is and I know that the parcel will rise until it reaches the surrounding air temperature. I am just not sure how or which formula I would use to solve the problem.

I'm having a bit of trouble figuring out a solution to this problem:

There is an isothermal layer of air which has a temperature of 0 °C extending from the surface to 1 km height. A parcel is 0.5 °C is released at the surface in the isothermal layer. How high does the parcel rise before it descends back?

I know what an isothermal layer is and I know that the parcel will rise until it reaches the surrounding air temperature. I am just not sure how or which formula I would use to solve the problem.

3 Body clean-up
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So I'm having a bit of trouble with how I would figure thisfiguring out. a solution to this problem:

There is an isothermal layer of air which has a temperature of $0$ degrees Celsius extending from the surface to $1$ km height. A parcel is $0.5$ degrees Celsius is released at the surface in the isothermal layer. How high does the parcel rise before it descends back?

I know what an isothermal layer is and I know that the parcel will rise until it reaches the surrounding air temperature. I am just not sure how or which formula I would use to figure this out.

Any help would be greatly appreciatedsolve the problem.

So I'm having a bit of trouble with how I would figure this out.

There is an isothermal layer of air which has a temperature of $0$ degrees Celsius extending from the surface to $1$ km height. A parcel is $0.5$ degrees Celsius is released at the surface in the isothermal layer. How high does the parcel rise before it descends back?

I know what an isothermal layer is and I know that the parcel will rise until it reaches the surrounding air temperature. I am just not sure how or which formula I would use to figure this out.

Any help would be greatly appreciated.

I'm having a bit of trouble figuring out a solution to this problem:

There is an isothermal layer of air which has a temperature of $0$ degrees Celsius extending from the surface to $1$ km height. A parcel is $0.5$ degrees Celsius is released at the surface in the isothermal layer. How high does the parcel rise before it descends back?

I know what an isothermal layer is and I know that the parcel will rise until it reaches the surrounding air temperature. I am just not sure how or which formula I would use to solve the problem.

2 Added Homework tag.
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