the depression turned northwestward toward Mozambique as thunderstorms increased, aided by a decrease in wind shear through a shift in the jet stream. The center came very close to the Mozambique coast near Inhambane. Due to the small radius of maximum winds, the coastline was spared from strong gusts, although the system dropped of rainfall in Inhambane over 48 hours. The storm turned toward the east on April 11 away from land. Convection organized thereafter into an eye feature, but was weaker than thunderstorms in typical tropical cyclones, resulting in its subtropical classification. The MFR estimated peak 10‑minute winds of on April 12, noting that the system should have been named, but also that its "structure has had no recent analogue in [the basin]." Meanwhile, the JTWC issued three Tropical Cyclone Formation Alerts, but never issued advisories. An increase in wind shear deteriorated the eye feature and the convection, promptly causing weakening. On April 15, the circulation dissipated off the southwest coast of Madagascar. Moderate Tropical Storm Innocente The final storm of the year had its origins in the Australian basin. An area of convection persisted on April 8 to the southwest of Indonesia, developing a distinct center two days later while moving to the west. However, the thunderstorms were unable to organize due to wind shear. On April 11, the MFR estimated that the system became a tropical disturbance, although since it was east of 90° E the agency did not issue advisories at that time. On the next day, the system crossed into the basin and was classified as Tropical Disturbance 14. Over the next few days, the convection waxed and waned, with the strongest winds in the northern periphery. On April 14, the JTWC began tracking the system as Tropical Cyclone 26S. The disturbance maintained a general west-southwest trajectory, influenced by a ridge to the south. After slowing down and encountering a more favorable environment, the system intensified into Moderate Tropical Storm Innocente on April 17, reaching peak 10‑minute winds of . Operationally, the MFR upgraded Innocente to storm status a day earlier, only to downgrade and re-upgrade; it was maintained as a depression during this time. The return of wind shear again caused weakening, beginning on April 18. A weak circulation persisted for several days, turning to the northwest with brief increases in thunderstorms. On April 24, Innocente dissipated, although the circulation drew moisture from the