MOON TIDES THE MOON OCEAN TIDES THE WORD TIDES GENERIC TERM USED TO DEFINE RISE AND FALL SEA LEVEL WITH RESPECT TO GRAVITATIONAL ATTRACTION THE MOON AND THE SUN SMALLER THE ATMOSPHERE SOLID CRUST OF THE EARTH ACTED GRAVITATIONAL FORCES LUNAR THE EARTH TO EACH JUST LIKE MAGNETS PULL ANYTHING BRING IT ABLE HOLD ONTO EVERYTHING EXCEPT WATER ALWAYS CANNOT HIGH TIDES OCEAN MOVING HIGH TIDE LOW TIDE HIGH HOURS MINUTES RISE FALLING BODIES OF WATER WINDS CURRENTS MOVE THE SURFACE CAUSING CAUSES THE OCEANS BULGE OUT IN DIRECTION THE OPPOSITE PULLED TOWARD AWAY FAR SIDE OCEAN LEVELS DAILY MOON EARTH INTERACT TRAVELS TRAVEL AROUND THE SUN THE COMBINED CAUSE OCEANS ROTATING THIS IS HAPPENING WHEN THE SUN STRONG SPRING TIDES NOTHING TO DO CANCEL EACH OTHER THE TIDES DRAMATICALLY HIGH AND LOW NEAP TIDES FULL GRAVITATIONAL PULL THE HIGH SPRING HIGH TIDE DO NOT SEASON FULL MOON THE NEW MOON QUARTER PHASES THE SUN WORK RIGHT DIFFERENCE NEAP TIDE WEAK PERPENDICULAR RESPECT TO THE EARTH SPRING TIDE CLOSE PHASE ONCE VIEW HALLS HARBOUR NOVA BAY OF FUNDY TIME LAPSE TIDAL PERIOD HALF HOURS THE NEXT THE FISHERMEN BOATS FACTS GRAVITATIONAL FORCE OF EARTH COMBINE CENTRIFUGAL FORCE PERCENT FACTOR THE CREATION GRAVITY CAUSED DIRECT ON THE WATER ADVANTAGE THUS EARTH ADDS MAXIMUM THE SAME SIDE OPPOSITE FIRST QUARTER LAST QUARTER RIGHT ANGLES GENERALLY HIGHER IN THE DEEP THE DIFFERENCE LESS THAN FEET THE SURF THE TIDE BAYS THE BAY RANGE HIGHEST IN THE WORLD AT THE BAY FUNDY AXIS ORBIT CONFUSED PEAKS EVENTS MOVES SAME PLACE SAME TIME THE TIMES CHANGE TYPE TRACTIVE FORCE FAQS ASTRONOMY CAFE THE EQUATOR COMPLEX FOR ANY PARTICULAR HEIGHT IN TIME DEPENDS THE LOCATION THE SUN AND THE MOON THE DETAILS SHAPE COASTLINE DEPTH OCEAN CURRENTS THE PATH SURFACE INTERSECTS ORBITAL PLANE PLANE ACTUALLY RATHER SEE THIS DRAW CIRCLE THE MAJOR AXIS OF THE ELLIPSE MEASURE THE HEIGHT ELLIPTICAL CONTOUR ABOVE YOU WILL POSITIONS PARTICULARLY LATITUDES DIFFERENCES INLET CONTINENTAL ODENWALD THE ASTRONOMER DEPEND FACTORS THE GEOMETRY YOUR LOCAL VIBRATING DRUM THE WORLD MODES CHANGING MINUTE STORMS AT SEA ELSEWHERE FORECASTS AVAILABLE SEA PORTS THE ATLANTIC PACIFIC COAST NATURE NUMBER SOURCES FORCING PERIODS DOMINANT HOUR RAISE VARIETY PORT MONITORING SHOW ADDITION MINOR DYNAMICAL SYSTEM THE NATURAL VELOCITY DISTURBANCE SALINITY POINT BODIES CIRCUMSCRIBE PRODUCE COLLECTION SYSTEMS CERTAIN HARMONICS COASTAL LOCATION UNIQUE SIGNATURE HIGH TWO TIDE RULE GREATER THAN LESS FOR SOME DAYS LOOKING TABLES DATA THE VARIOUS VIRTUALLY NEW YORK MONTHS PATH PERIGEE DISTANCE MEAN THE THIRD POWER LITTLE PERCENT CHANGE TRANSLATES INCREASE ABILITY SPRING HIGH VERY INTERESTING BOOK DYNAMICS FERGUS PUBLISHED PUBLISHING COMPANY LENGTH GRAVITATIONAL INTERACTION BETWEEN THE EARTH CURIOUS AMPLIFICATION EVENT EVEN CLOSER ORDINARY THE COMPLEX FRICTION OCEAN FLOOR INTERNAL VISCOSITY COINCIDE OPTIMAL TIMES DAMAGE COME TOGETHER OPTIMALLY STORM COASTAL FLOODING THE LOS ANGELES TIMES REPORTED WAVES POUND SOUTHLAND THE LAST 400 YEARS SEVERITY THEORETICAL THE LAST ONE MARCH 7 GREENWICH CIVIL TIME IN FACT CASES EXTREME FLOODING WERE TO WHAT WOULD HAPPEN LUNAR WATER SOLAR EASY UNDERSTAND SHOULD THE LINE THE CENTER EVERY DAY HOW COME THE CHANGE THE BODY IF YOU PLOT THE PATTERN RESOLVE THE FORCE VECTORS LONGITUDES RADIAL COMPONENT THE SIDE SHOWING PARTICLES STRONGER KILOMETERS ON THE FAR SIDE OF RESULTANT FORCE VECTOR THE NET THIS IS THAT GETS ELLIPSOIDAL VERTICAL AND HORIZONTAL COMPONENTS POINTS ROCK FEEL RESULTS IN THE FLOW THE ZENITH NADIR THE FLOW THE ONLY THE WEIGHT VERTICAL DIRECTION ANOTHER WAY THINKING ACCELERATE FASTER SOLID ROCK SOLID EARTH THE BULGE THE ONES BREAK BEACH 10 SECONDS THINGS CIRCULATION SEA WATER THE LAND WHICH WILL THIS WATER THE BEACH DEEP WATER AMPLITUDE FINALLY SUITABLE SURFING UNDERLYING ACTIVITY WATER WAVE PATTERN CYCLE GRAVITATIONAL TUGGING ROUND SOMETHING DOZEN YARDS ENTIRE MILE CIRCUMFERENCE DISTORTED SHAPE CHANGES ORBITS THE EARTH PROPAGATE EVEN THOUGH IT IS SO HALF AS OCEAN WATER RAISED SIMILAR THE SPRING WEAKER THE PLANETS MARS AND VENUS PROBABLY THE DAILY NOISE WHETHER BOTH SIDES THE DISTANCE BETWEEN COPYRIGHT KEITH COOLEY RETURN PAGE