A tropical wave emerged from the west coast of Africa on August 30 and tracked westward across the Atlantic Ocean, maintaining a vigorous area of convection along the wave axis.
By September 1 most of the  deep convection had been stripped away by southwesterly wind shear.
 Despite this, the wave remained well-defined as it continued west-northwest.
The wave split into two pieces; the northern portion passed between the Leeward Islands and Hurricane Maria on September 3, while the southern portion moved into the Caribbean Sea.
On September 4, the northern portion of the wave began to interact with an upper-level low pressure system and an elongated trough that was located between Bermuda and the Leeward Islands—the same trough which contributed to the development of Hurricane Ophelia.
As a result of the low wind shear, convection redeveloped and organized along the wave axis.
Convective banding formed around a broad surface low.
It is estimated that the system developed into a tropical depression at 1800 UTC on September 5.
At the time it was located approximately 350 miles (560 km) to the south-southwest of Bermuda.

Upon being designated, Tropical Depression Fifteen developed deep convection close to, and to the east of, the center of circulation.
At the same time, banding features became better organized.
Later on September 5, the overall cloud pattern improved while thunderstorm activity condensed and deepened within the increasingly well-defined circulation.
Just six hours after being designated as a tropical depression, the cyclone intensified into a tropical storm; it was given the name Nate by the National Hurricane Center.
Over the following two days, Nate drifted slowly northeastward towards Bermuda.

Within the early hours of September 6, Nate became quasi-stationary under a weak steering pattern between Hurricane Maria and a disturbance over The Bahamas.
Satellite imagery indicated that the cloud pattern continued to organize with excellent outflow surrounding the storm.
Late on September 6 a developing banding eye feature became evident.
Tropical Storm Nate strengthened further and became a hurricane at 1200 UTC on September 7, as it began to turn away from Bermuda.
Some models indicated that Nate could have been either absorbed by or merged with the larger Hurricane Maria, but the National Hurricane Center (NHC) forecast that Nate would survive as a separate system, which it did.
The large low to the northeast of The Bahamas gradually opened into a broad trough as a shortwave trough approached from the northwest.
The larger trough slowly became elongated in a northeast–southwest manner late on September 7.
At the same time, the shortwave trough moved southward along the west side of the other trough.
The increasing southwesterly flow along the southeast side of the broad trough caused Nate to accelerate northeastward.
Nate reached its peak intensity of 90 mph (145 km/h) late on September 8 as it passed 120 miles (205 km) southeast of Bermuda, while its strongest winds remained well offshore.

While at peak intensity, the storm maintained a well-organized and "impressive" convective pattern.
Soon after the storm peaked in strength, increasing wind shear and dry air caused Nate to weaken back into a tropical storm later on September 9.
Satellite imagery showed that the cloud pattern began to rapidly deteriorate.
The hurricane was downgraded to a tropical storm at 1800 UTC on September 9 and continued to weaken as wind shear increased in association with an approaching trough and a related cold front.
By late on September 9, all of the already limited convective activity was confined to the eastern semicircle, leaving the low-level center exposed.
The storm was reduced to a swirl of low-level clouds just hours later.
Nate became extratropical the next day before becoming absorbed by a larger system by 0000 UTC on September 13, to the north-northeast of the Azores.
A tropical wave emerged from the west coast of Africa on August 30 and tracked westward across the Atlantic Ocean, maintaining a vigorous area of convection along the wave axis. By September 1 most of the  deep convection had been stripped away by southwesterly wind shear.  Despite this, the wave remained well-defined as it continued west-northwest. The wave split into two pieces; the northern portion passed between the Leeward Islands and Hurricane Maria on September 3, while the southern portion moved into the Caribbean Sea. On September 4, the northern portion of the wave began to interact with an upper-level low pressure system and an elongated trough that was located between Bermuda and the Leeward Islands—the same trough which contributed to the development of Hurricane Ophelia. As a result of the low wind shear, convection redeveloped and organized along the wave axis. Convective banding formed around a broad surface low. It is estimated that the system developed into a tropical depression at 1800 UTC on September 5. At the time it was located approximately 350 miles (560 km) to the south-southwest of Bermuda.
Upon being designated, Tropical Depression Fifteen developed deep convection close to, and to the east of, the center of circulation. At the same time, banding features became better organized. Later on September 5, the overall cloud pattern improved while thunderstorm activity condensed and deepened within the increasingly well-defined circulation. Just six hours after being designated as a tropical depression, the cyclone intensified into a tropical storm; it was given the name Nate by the National Hurricane Center. Over the following two days, Nate drifted slowly northeastward towards Bermuda.
Within the early hours of September 6, Nate became quasi-stationary under a weak steering pattern between Hurricane Maria and a disturbance over The Bahamas. Satellite imagery indicated that the cloud pattern continued to organize with excellent outflow surrounding the storm. Late on September 6 a developing banding eye feature became evident. Tropical Storm Nate strengthened further and became a hurricane at 1200 UTC on September 7, as it began to turn away from Bermuda. Some models indicated that Nate could have been either absorbed by or merged with the larger Hurricane Maria, but the National Hurricane Center (NHC) forecast that Nate would survive as a separate system, which it did. The large low to the northeast of The Bahamas gradually opened into a broad trough as a shortwave trough approached from the northwest. The larger trough slowly became elongated in a northeast–southwest manner late on September 7. At the same time, the shortwave trough moved southward along the west side of the other trough. The increasing southwesterly flow along the southeast side of the broad trough caused Nate to accelerate northeastward. Nate reached its peak intensity of 90 mph (145 km/h) late on September 8 as it passed 120 miles (205 km) southeast of Bermuda, while its strongest winds remained well offshore.
While at peak intensity, the storm maintained a well-organized and "impressive" convective pattern. Soon after the storm peaked in strength, increasing wind shear and dry air caused Nate to weaken back into a tropical storm later on September 9. Satellite imagery showed that the cloud pattern began to rapidly deteriorate. The hurricane was downgraded to a tropical storm at 1800 UTC on September 9 and continued to weaken as wind shear increased in association with an approaching trough and a related cold front. By late on September 9, all of the already limited convective activity was confined to the eastern semicircle, leaving the low-level center exposed. The storm was reduced to a swirl of low-level clouds just hours later. Nate became extratropical the next day before becoming absorbed by a larger system by 0000 UTC on September 13, to the north-northeast of the Azores.
Hurricane Nate (2005)