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Perigean Spring Tides
Predicting Potential Disasters: How Tidal
Information May Save You From a Coastal Crisis
August 1998
The memorable blizzard of February, 1978, caused
coastal flooding and $500 million in damages to Massachusetts alone,
much of the loss to coastal properties. The storm began a few hours
after the moon was in perigee (closest to the earth) on February
6, and the day before a new moon. The property damage resulted not
only from the severity of the storm and its accompanying storm surge,
but also from the extreme high water caused by the nearly coincident
new moon tide, or "spring tide," and a perigean tide.
Though meteorological conditions, such as those
that produced the Blizzard of '78, are predictable only days or
hours in advance, astronomical high tides are predictable centuries
in advance. If you are a coastal property owner in Massachusetts,
or a boat owner, you may want to note dates on your calendar when
a perigean high tide is predicted, as it could combine with a storm
to produce coastal flooding and property damage. You can find the
dates for perigean tides -- and information about tides and tidal
ranges in general -- in several reference materials that are listed
in this bulletin.

Perigean Spring Tides
The term "spring tide" does not refer to the season,
but rather to the higher high tides and lower low tides which occur
at new and full moons. At new and full moons, the sun, earth and
moon are aligned such that the pull of the sun on the oceans adds
to the pull of the moon on the oceans. Spring tides alternate at
one week intervals with "neap tides." Neap tides occur
during the first or third quarter moons when the sun and moon are
aligned at right angles with respect to earth, and the sun tides
subtract from the moon tides.
A perigean tide refers to a tide that occurs when the moon is closest
to the earth. The moon's orbit around the earth is elliptical rather
than circular, which means that the distance between earth and moon
is always changing. Perigee refers to the time when the moon and
the earth are closest to one another. At perigee, the moon is about
30,000 miles closer to earth than at apogee, when the moon is farthest
from earth. Perigee is reached about once a month, roughly the time
it takes for the moon to revolve around the earth. When the moon
is closest to earth, its effect on tides is greatest.
The largest astronomical tides, perigean spring tides, occur when
spring tides and perigean tides coincide. Perigean spring tides
occur at intervals that are slightly more than six months long,
so each year they are later in the season than the preceding year.
For this reason, we must refer to tables of predicted tides to know
exactly when to expect these unusually high tides.
The term "storm surge" denotes the high sea levels --
those not related to astronomical tides -- that often accompany
severe storms. There are two major causes of storm surges: strong
onshore winds the low atmospheric pressure accompanying such storms.

As in the Blizzard of '78, major coastal flooding and storm damage
is likely to occur when perigean spring tides coincide with a major
storm and storm surge. The direction of the wind (onshore) and low
atmospheric pressure (which effectively contributes to a higher
sea level) will add to the severity of storm damage. Because Massachusetts
has coastline facing the ocean at virtually every point of the compass
rose, coastal flooding during storms is likely to occur somewhere
regardless of the direction of the wind. The role of tides in increasing
storm damage is more significant in areas having larger tidal ranges
(i.e., the North and South Shores, Boston, Cape Cod Bay and the
open ocean side of outer Cape Cod) than in areas with smaller tidal
ranges (i.e., the south shore of Cape Cod, Buzzards Bay, Nantucket,
Martha's Vineyard, Fairhaven, and New Bedford).
While damaging storms can occur under other sea and tidal conditions,
high astronomical tides caused by the near coincidence of a spring
tide and perigee can be especially dangerous. By becoming more informed
of the timing of these predictable events, you will also be preparing
yourself for the unpredictable events of nature.
Sources of Tidal Data for Mariners and Coastal Residents
Massachusetts coastal residents, fishers, shellfishers, aquaculturists,
and mariners need to know the times and heights of high and low
tides. Some harbors, for example Wellfleet and Barnstable, do not
have enough water to allow passage of vessels at low tide. In other
places, rocks are a hazard to boats during some parts of the tidal
cycle. Knowledge of tidal cycles and tidal currents is critical
for planning trips and for operating vessels safely.
In 1890, the federal government began to publish both high and
low water data annually. In 1995, the National Ocean Service (NOS)
redefined its role to be maintaining and updating the tidal predictions
database and published its last hard copy volumes of Tide Tables
and Tidal Currents. Currently, tidal data are available on-line
through the National Oceanic and Atmospheric Administration (NOAA)
website, http://www.noaa.gov
and from several private publishers who utilize NOS databases. The
website lists tidal forecasts for the next four days. For long-term
tide predictions, you can call the NOS office at (301) 713-2815
between 7 a.m. and 3 p.m. EST. You may also request long term tide
predictions by e-mailing: ipss@ceob.nos.noaa.gov.
If you submit your request by e-mail, include: your full name, your
postal mailing address, your phone number including area code, the
location(s) for which you want predictions, the format and options
you desire (see NOAA website for available formats and options).
The fee for these services is $31 per year for predictions at one
location; add $10 for a year of predictions at each additional location.
Although NOS ceased publishing tide and tidal currents volumes
with the 1995 editions, NOS makes its data available to commercial
publishers who continue the tradition of hard copy volumes of tides
and tidal currents for coastal waters. The three publishers that
NOAA recognizes as publishing complete tidal references using NOAA
data are:
ProStar Publications
East Coast: 3 Church Circle, Suite 109, Annapolis, MD 21401
(800) 481-6277
West Coast: 13486 Beach Avenue, Marina Del Rey, CA 90292
(800) 481-6277
Reed's Nautical Almanacs
Thomas Reed Publications, Inc., 13A Lewis Street, Boston, MA 02113
(800) 995-4995
International Marine
P.O. Box 182607, Columbus, OH 43218-2607
(800) 262-4729
NOTE: These volumes are available from their publishers as well
as marine suppliers. The list price of Reed's Nautical Almanacs,
which include both tide and current tables, is $29.95. Reed's also
includes the Coast Pilot and Light List and a complete nautical
ephemeris. Both ProStar Publications and International Marine, a
division of McGraw-Hill, publish separate volumes for tides and
currents by region. Each volume costs $13.95.
In addition to the official NOS data, many navigators in the northeast
use the Eldridge Tide and Pilot Book which was first published in
1854 as Eldridge's Pilot for Vineyard Sound and Monomoy Shoals;
the Tide and Pilot Book followed in 1875. The 1998 Eldridge Tide
and Pilot Book costs $9.95.
Many coastal residents, boaters, and beachgoers use weekly tide
tables from local newspapers or yearly tide tables provided by local
fishing supply and hardware stores. Many fishers and boaters use
NOAA's National Weather Service radio broadcasts which give tidal
information as well as wind and sea conditions. An inexpensive dedicated
receiver may be purchased at home electronics stores or marine suppliers.
Many VHF marine radios receive the weather channel.
More about Tides
In addition to tidal and current predictions, readers who want
more information on how tides work can find a clearly presented
summary of tidal theory at the NOAA website: http://www.noaa.gov
or consult the sources below.
Sources
- Willard Bascom. 1980. Waves and Beaches, pp. 92-104.
- Edward P. Clancy. 1968. The Tides: Pulse of the Earth.
- Eldridge Tide and Pilot Book, 1998.
- William T. Fox. 1983. At the Sea's Edge: An Introduction to
Coastal Oceanography for the Amateur Naturalist, pp. 94-106.
- NOAA, National Ocean Service, Office of Coast Survey. "Our
Restless Tides: A Brief Explanation of the Basic Astronomical
Factors which Produce Tides and Tidal Currents," http://www.opsd.nos.noaa.gov/predtide.html
- 1998 NOAA Tide and Tidal Current Tables, International Marine.
- Reed's Nautical Almanac: North American East Coast, 1998
For more information about the research or outreach projects profiled
in the Marine Extension Bulletin, contact WHOI Sea Grant at (508)
289-2398 or seagrant@whoi.edu.
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