A northwest wind.

At Woodstock, the penultimate of August.

A couple of ghosts haunt the old, burnt-down house.

As for the Pacific, the unknown size of the Indonesian Throughflow complicates quantitative estimates of heat transport divergence in the Indian Ocean. Because the Throughflow entering the Indian Ocean is warm (about 20°C) relative to its temperature as it exits the Indian Ocean across the southern boundary at 32°S, the overall effect of the Throughflow is to lead to an ocean heat transport convergence over the Indian Ocean.