But when the surface temperature drops below $4^\circ C$ (here it is $2^\circ C$), the water near the surface is less dense than the warmer water below.
Hence the downward flow ceases, the water at the bottom remains at $4^\circ C$ until nearly the entire lake, is frozen.

$(i)$ a body with large reflectivity is a poor emitter
$(ii)$ a brass tumbler feels much colder than a wooden tray on a chilly day
$(iii)$ the earth without its atmosphere would be inhospitably cold
$(iv)$ heating systems based on circulation of steam are more efficient in warming a building than those based on circulation of hot water