Assertion (A) : Average ocean salinity generally decreases from equator the pole but tropical zone (20° - 30°) is charcterized by maximum salinity.
Reason (R) : The tropical zone owes its high salinity to high temperature, high evaporation and significantly low rainfall.
Codes :

Question

Assertion (A) : Average ocean salinity generally decreases from equator the pole but tropical zone (20&deg; - 30&deg;) is charcterized by maximum salinity.
Reason (R) : The tropical zone owes its high salinity to high temperature, high evaporation and significantly low rainfall.
Codes :

Admin · Accepted Answer

Both (A) and (R) are true and (R) is the correct explanation of (A)

Admin · Answer

Both (A) and (R) are true but (R) is not a correct explanation of (A)

Admin · Answer

(A) is true but (R) is false

Admin · Answer

(A) is false but (R) is true

Q. Assertion (A) : Average ocean salinity generally decreases from equator the pole but tropical zone (20° - 30°) is charcterized by maximum salinity.
Reason (R) : The tropical zone owes its high salinity to high temperature, high evaporation and significantly low rainfall.
Codes :

Discusssion

Q. Assertion (A) : Average ocean salinity generally decreases from equator the pole but tropical zone (20° - 30°) is charcterized by maximum salinity. Reason (R) : The tropical zone owes its high salinity to high temperature, high evaporation and significantly low rainfall. Codes :

Discusssion

Q. Assertion (A) : Average ocean salinity generally decreases from equator the pole but tropical zone (20° - 30°) is charcterized by maximum salinity.
Reason (R) : The tropical zone owes its high salinity to high temperature, high evaporation and significantly low rainfall.
Codes :