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The second option is to make Ryu dodge, by rolling away from the attack in a maneuver called "reverse wind".
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As discussed in Sun (2013), the zone of the weak (or reverse) winds in the mid-level (5 km ~ 10 km) creates a new blocking as an artificial steep mountain for the westerly flow in z = 7 ~ 8 km.
The landlocked character of the ocean along its northern boundary and the resultant seasonally reversing wind and sea surface circulation patterns are features unique to the IO.
In winter the situation is reversed: winds blow predominantly from the north, bringing with them cold, dry air from the continent.
The modern SAM is an atmospheric circulation pattern with reversing winds during the winter and the summer monsoon.
Episodes of reverse winds can occur during both seasons.
On the north side, with the reversing wind behind him, he used the wind as an ally, brushing up on the ball to control it, waiting for a shorter ball to flatten out and hurt Nadal.
That was time you could even reverse, by winding back the clock or tipping the hourglass over.
The slanting strips of strong and weak (or reverse) westerly winds in z > 10 km resemble the propagating mountain waves.
The first zone, extending north from latitude 10° S, has a monsoon climate (characterized by semiannual reversing winds).
It is subject to greater seasonal variability than any other ocean basin on the globe [ 41, 42], with seasonally reversing monsoon winds inverting its circulation completely on a biannual basis [ 43, 44].
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