On January 10, the JMA reported that a tropical depression had developed, about 1,800 km (1,120 mi) to the southeast of Manila, Philippines.
The JMA expected the system to develop into a tropical storm within 24 hours, despite it being located in an area of marginal conditions for further development.
Under moderate vertical wind shear, the system became highly sheared on the next day, although strong northeasterly trade wind surges and a good westward outflow enhanced by the strong easterly upper-level winds were helping to sustain the associated convection.
On January 12, the JMA no longer expected a tropical storm and even downgraded the tropical depression to a low-pressure area late on the same day, when convection became more disorganized.

The low-pressure area crossed Mindanao, Philippines from the south on January 13 and emerged into the area off the northeast coast of Mindanao on the next day.
Although the JMA operationally upgraded the system back to a tropical depression on January 14, the RSMC best track data indicated that the tropical depression had not persisted until 00:00 UTC on January 15, with the poor structure under high vertical wind shear and strong northeasterly surges.
After the system slowly drifted west-northwestward and then southwestward, the JMA began to issue warnings on the tropical depression at noon on January 16, albeit not expecting it to intensify into a tropical storm.
Soon, the Joint Typhoon Warning Center (JTWC) issued a Tropical Cyclone Formation Alert on the system, for the consolidating and slightly better defined low-level circulation center, favorable sea surface temperature, moderate vertical wind shear, as well as highly diffluent outflow.

Early on January 17, the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) upgraded the system from a low-pressure area to a tropical depression and assigned the local name Agaton, when the system was partially exposed with flaring deep convection along the northwestern quadrant.
The JMA upgraded the tropical depression to a tropical storm about 210 km (130 mi) east of Surigao City and named it Lingling at 00:00 UTC on January 18, shortly before the JTWC upgraded the system to a tropical depression.
Lingling's central convection and the banding associated with a partially exposed low-level circulation center have become improved, when the storm started to drift southward away from a strong northeasterly surge in a weak steering environment.
Six hours later, the JTWC upgraded Lingling to a tropical storm, based on the scatterometer data and Dvorak estimates.

However, half a day later, the JTWC downgraded Lingling to a tropical depression as its deep central convection was diminishing under the influence of moderate to strong vertical wind shear.
Lingling began to accelerate south-southeastward under the influence of the strong northeasterly surge flow on January 19, and was struggling to consolidate due to the marginally favorable upper-level conditions.
Late on the same day, the JTWC issued the final warning on Lingling, as the infrared satellite imageries depicted an exposed, weakening low-level circulation center with isolated,
flaring convection sheared to the northwest.
A ship observation at 15:00 UTC, 72 nautical miles (133 km; 83 mi) north-northeast of the system, reported winds at only 10 knots (20 km/h; 10 mph) with atmospheric pressure of 1,013 hPa (29.9 inHg).

During January 20, the JMA reported that the system weakened into a tropical depression, before the system was last noted later that day as it dissipated to the southeast of the Philippines.
On January 10, the JMA reported that a tropical depression had developed, about 1,800 km (1,120 mi) to the southeast of Manila, Philippines. The JMA expected the system to develop into a tropical storm within 24 hours, despite it being located in an area of marginal conditions for further development. Under moderate vertical wind shear, the system became highly sheared on the next day, although strong northeasterly trade wind surges and a good westward outflow enhanced by the strong easterly upper-level winds were helping to sustain the associated convection. On January 12, the JMA no longer expected a tropical storm and even downgraded the tropical depression to a low-pressure area late on the same day, when convection became more disorganized.
The low-pressure area crossed Mindanao, Philippines from the south on January 13 and emerged into the area off the northeast coast of Mindanao on the next day. Although the JMA operationally upgraded the system back to a tropical depression on January 14, the RSMC best track data indicated that the tropical depression had not persisted until 00:00 UTC on January 15, with the poor structure under high vertical wind shear and strong northeasterly surges. After the system slowly drifted west-northwestward and then southwestward, the JMA began to issue warnings on the tropical depression at noon on January 16, albeit not expecting it to intensify into a tropical storm. Soon, the Joint Typhoon Warning Center (JTWC) issued a Tropical Cyclone Formation Alert on the system, for the consolidating and slightly better defined low-level circulation center, favorable sea surface temperature, moderate vertical wind shear, as well as highly diffluent outflow.
Early on January 17, the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) upgraded the system from a low-pressure area to a tropical depression and assigned the local name Agaton, when the system was partially exposed with flaring deep convection along the northwestern quadrant. The JMA upgraded the tropical depression to a tropical storm about 210 km (130 mi) east of Surigao City and named it Lingling at 00:00 UTC on January 18, shortly before the JTWC upgraded the system to a tropical depression. Lingling's central convection and the banding associated with a partially exposed low-level circulation center have become improved, when the storm started to drift southward away from a strong northeasterly surge in a weak steering environment. Six hours later, the JTWC upgraded Lingling to a tropical storm, based on the scatterometer data and Dvorak estimates.
However, half a day later, the JTWC downgraded Lingling to a tropical depression as its deep central convection was diminishing under the influence of moderate to strong vertical wind shear. Lingling began to accelerate south-southeastward under the influence of the strong northeasterly surge flow on January 19, and was struggling to consolidate due to the marginally favorable upper-level conditions. Late on the same day, the JTWC issued the final warning on Lingling, as the infrared satellite imageries depicted an exposed, weakening low-level circulation center with isolated,
flaring convection sheared to the northwest. A ship observation at 15:00 UTC, 72 nautical miles (133 km; 83 mi) north-northeast of the system, reported winds at only 10 knots (20 km/h; 10 mph) with atmospheric pressure of 1,013 hPa (29.9 inHg).
During January 20, the JMA reported that the system weakened into a tropical depression, before the system was last noted later that day as it dissipated to the southeast of the Philippines.
Tropical Storm Lingling (2014)