Answer:
it moderates coastal mid latitude temperatures.
Explanation:
North Atlantic Drift is the part of warm western limit current spilling out of Florida to north western Europe. This current is known as Gulf stream. This is thin, profound and warm current that reaches out along the eastern bank of the USA. Northern piece of this stream is known as North Atlantic Drift.
This warm current streams along the north-western beach front Europe and keeps the waterfront temperature higher than general in the winter months.
This present causes an expansion of about 5°C of the surrounding temperature than the temperature expected at a similar scope somewhere else. On the off chance that this current would have been missing, at that point the normal winter temperature of London would be 2°C.
In this way, the right answer for this situation will be, it moderates waterfront mid scope temperatures.