Upon becoming a tropical cyclone, Narda was located over warm sea surface temperatures.

As the depression headed gradually west-northwestward over extremely warm sea surface temperatures, it steadily intensified.

Accelerating to the southeast, the cyclone began to cross over cool sea surface temperatures and encountered wind shear.

The storm began weakening afterward, weakening to a depression on August 25 after moving over cool sea surface temperatures.

A tropical wave forming over sea surface temperatures of 23 degrees.

Despite being over warm sea surface temperatures, the depression dissipated the following day as wind shear began to significantly increase.

Despite belong located over warm sea surface temperatures, it failed to intensify.

Located over warm sea surface temperatures, the hurricane continued to improve in appearance on satellite images, as the barometric pressure within its eye steadily decreased.

Due to cool, dry air, the system initially did not intensify, although its passage over warmer sea surface temperatures on March 19 allowed for strengthening.

After moving over increasingly cool sea surface temperatures, the cyclone began to gradually weaken.