Tropical Storm Andres - May 31-June 6, 1997
- ️David Roth
The main belt of the Westerlies extended southward into the deep
tropics for most of May. Towards the
end of the month, the Westerlies briefly lifted northward, and a
surface circulation developed south of
southeast Mexico on May 30th, possibly due to a tropical wave which
emerged off the African coast
on May 14th. Deep convection became concentrated near its center
on the 31st, and it became a tropical
depression that evening. Initially, Andres drifted northwest as
it became a tropical storm, which forced
recurvature just shy of Mexico as it neared the Westerlies, and a weak
cold front approached from the north.
The system turned east-northeast between the 3rd and 5th, before
turning southeast thereafter as the flow
aloft became more northwesterly. The northwest winds aloft caused
vertical wind shear, which weakened
the cyclone. On the 6th, Andres drifted north as a tropical
depression, dissipating as it reached the coast of
El Salvador late that day. Below is its track, supplied by the
National
Hurricane Center.
The
graphics below show the storm total rainfall for Andres, which used
information from the Comision del
Agua, which contains Mexico's National Weather Service.