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Preliminary Report
Tropical Storm Arlene
11 - 18 June 1999

James L. Franklin
National Hurricane Center
7 July 1999

Tropical Storm Arlene
Tropical Depression Two
Hurricane Bret
Hurricane Cindy
Hurricane Dennis
Tropical Storm Emily
Tropical Depression Seven
Hurricane Floyd
Hurricane Gert
Tropical Storm Harvey
Tropical Depression Eleven
Tropical Depression Twelve
Hurricane Irene
Hurricane Jose
Tropical Storm Katrina
Hurricane Lenny

[1999 Atlantic Hurricane Season]

Arlene, the first tropical storm of the 1999 Atlantic hurricane season, spent its life at sea in the central Atlantic. Arlene passed roughly 100 n mi east of Bermuda, but did not bring tropical storm force winds to the islands.

a. Synoptic History

During its initial stages of development Arlene was not a purely tropical system. Although initially cold-core, by the time depression status had been attained on 11 June, the overall structure more-closely resembled a tropical, rather than a subtropical cyclone. At some (unknown) point, the system became warm-core, as revealed by reconnaissance data on the 15th.

Arlene's complex development can be traced to a mid- to upper-level cold low that developed near the tail end of a diffuse front in the central Atlantic. Water-vapor imagery first showed the circulation of the upper low a few-hundred miles north of Puerto Rico late on 8 June. Simultaneously, a fairly large-amplitude tropical wave passed through the tail end of the frontal zone southeast of the upper low, and a low-level cloud swirl became visible near 22N, 61W, close to the wave axis, and southeast of the upper low. The low-level cloud swirl then moved slowly north-westward over the next two days without development due to westerly shear from the upper low.

Throughout this period, fairly steady convection had been maintained in the diffluence region to the east of the upper low. By 0600 UTC on the 10th, the low-level circulation moved underneath the cold low, near 24N, 63W. Shortly thereafter, the upper low began to move off to the east into the convective area. As the upper low accelerated northeastward late on the 10th, satellite microwave imagery revealed the rapid downward development of a vortex in the convection, which led to the formation of a new low-level center. During the morning of the 11th, the convection acquired a well-defined banding pattern, and it is estimated that a tropical depression formed at 1800 UTC on the 11th, about 465 n mi southeast of Bermuda. The original low-level cloud swirl continued moving away to the west and gradually dissipated.

The best track locations and intensities for Arlene are given in Table 1, with the track plotted in Figure 1. Almost immediately after reaching depression status, the cyclone slowed and began a northward drift for 24 h. By 1200 UTC on the 12th, Dvorak satellite classifications from the Tropical Analysis and Forecast Branch (TAFB) of the Tropical Prediction Center and the NOAA/NESDIS Satellite Analysis Branch (SAB) indicated that tropical storm strength had been attained. Arlene intensified for 12 h until westerly shear began to expose the low-level circulation center. The maximum intensity was reached at 0000 UTC on the 13th, when the winds were estimated to be 50 kt and the minimum central pressure was estimated to be 1006 mb. From the 13th to the 15th, Arlene moved generally west-northwestward while weakening slightly under the westerly shear.

Steering currents became poorly defined and Arlene moved little on the 15th. The best track indicates that Arlene executed a small cyclonic loop, although this apparent motion may have been due a reformation of the center closer to the convection on the east side of the cyclone. A northwesterly motion resumed late on the 15th, followed by a gradual turn to the north then northeast over the next three days as Arlene moved around the western edge of the subtropical ridge. Arlene's closest approach to land was at 0600 on the 17th, when the cyclone passed about 100 n mi to the east of Bermuda. Convection began to diminish on the 16th as the environmental shear changed to northeasterly and Arlene moved over cooler waters. Synoptic-scale upper-level confluence and subsidence in the immediate environment of Arlene also acted to suppress convection. The low-level circulation weakened to depression status at 0000 UTC on the 17th, and dissipated ahead of an approaching frontal zone on the 18th.

b. Meteorological Statistics

Figures 2 and 3 show the best track curves of maximum sustained surface wind (defined as a 1 min average at an elevation of 10 m) and minimum central pressure, respectively, as well as the observations on which the best track estimates are based. There were no direct measurements of surface winds; the best track values are based on interpretation of Dvorak satellite classifications from TAFB, SAB, and the Air Force Weather Agency (indicated by AFGWC in figure legends), as well as reductions of (mostly near 1000 ft) flight-level reconnaissance winds.

There was only a limited amount of in-situ aircraft reconnaissance data from the Air Force Reserve Hurricane Hunter Squadron, from 1200 UTC on the 15th to 0000 UTC on the 17th. The maximum winds from the reconnaissance aircraft were observed from 15/1200-16/0600 UTC, when the surface winds were estimated to be 45 kt (Figure 2). As is typical for storms in the subtropics, central pressures measured by reconnaissance were somewhat higher than satellite-based estimates (Figure 3). Arlene's minimum central pressure is estimated from satellite imagery and ship reports to be 1006 mb at 13/0000 UTC, although the lowest pressure measured by aircraft reconnaissance was 1008 mb at 15/1200 UTC.

There are no known ship or land reports of winds in excess of 34 kt associated with Arlene.

c. Casualty and Damage Statistics

There have been no reports of casualties or damage from Arlene.

d. Forecast and Warning Critique

Official forecast track errors for Arlene were 30, 55, 89, 101, and 99 n mi, for the 12, 24, 36, 48, and 72 h forecasts, respectively. These errors are 30%-60% lower than the average official Atlantic basin errors for the period 1989-1998. Early forecasts did not capture the sharp turn to west. The recurvature path was fairly well forecast, although there was a slight westward bias (in the direction of Bermuda).

Arlene's intensity was generally overforecast, but with errors comparable to the 1990-1997 period average. Arlene was briefly forecast to become a hurricane. Intensity forecast errors during the second half of Arlene's track were very low.

Tropical storm watches and warnings (Table 2) were issued for Bermuda; however, Arlene passed sufficiently far to the east that no significant weather affected the islands.

Figure 1. Best track positions for Tropical Storm Arlene, 11-18 June 1999.

Figure 2. Best track maximum sustained wind speed curve for Tropical Storm Arlene.

Figure 3. Best track minimum central pressure curve for Tropical Storm Arlene.

Table 1. Best track for Tropical Storm Arlene, 11-18 June 1999.
Position Pressure
Wind Speed
Lat. (°N) Lon. (°W)
11/180027.158.1101030tropical depression
12/120028.357.3100935tropical storm
17/000031.862.8101430tropical depression
13/000028.857.5100650minimum pressure

Table 2. Watch and warning summary for Tropical Storm Arlene, June 1999.
Action Location
14/1500tropical storm watch issuedBermuda
16/0600tropical storm warning issuedBermuda
17/0900tropical storm warning discontinuedBermuda


Last updated February 2, 2000