Step 1: What forms deep water?
Deep water masses form by convection where surface water becomes dense enough to sink. Density increases with low temperature and high salinity.
Step 2: North Atlantic Deep Water (NADW).
In the North Atlantic, especially near the Labrador and Greenland Seas, cold surface temperatures and brine rejection from sea ice formation create very dense water.
Step 3: Exclude wrong options.
- (A) Low T + Low S → not dense enough.
- (B) High T + High S → warm, less dense.
- (C) High T + Low S → least dense of all.
- (D) Low T + High S → very dense, sinks to form NADW.
Final Answer:
\[
\boxed{\text{Low temperature and high salinity}}
\]