DOKUZ EYLUL UNIVERSITY SCHOOL OF MARITIME BUSINESS AND MANAGEMENT DEPARTMENT OF DECK S elçuk N as SELÇUK NAS TIDE & TIDE DIAMOND
DOKUZ EYLUL UNIVERSITY SCHOOL OF MARITIME BUSINESS AND MANAGEMENT DEPARTMENT OF DECK S elçuk N as SELÇUK NAS TIDE Vertical rise and fall of the surface of a body of water caused primarily by the differences in gravitational attraction of the moon, and to a lesser extent of the sun, upon different parts of the earth. Moon is many times closer to the earth than the sun therefore gravitational pull is 2 1/4 times more pronounced
DOKUZ EYLUL UNIVERSITY SCHOOL OF MARITIME BUSINESS AND MANAGEMENT DEPARTMENT OF DECK S elçuk N as SELÇUK NAS What Causes Tides Strong gravitational pull of the moon on the side of the earth nearest the sun, Strong outward centrifugal force generated by the earth-moon system on the opposite side of the earth, Cause the water on the earth’s surface to bulge out in the form of high tides on both sides. The same phenomenon occurs between the sun and the earth but on a much smaller scale. The moon revolves around the earth once each month. Lunar or Tidal day - 24 hrs and 50 min Earth rotates beneath it in the same direction. Most locations on earth experience four tides per day. Each successive high and low tide constitutes one tide cycle. Tide patterns are distorted from the normal 4-tide pattern because of the effects of land masses, constrained waterways, friction, the Coriolis effect, and other effects.
DOKUZ EYLUL UNIVERSITY SCHOOL OF MARITIME BUSINESS AND MANAGEMENT DEPARTMENT OF DECK S elçuk N as SELÇUK NAS
DOKUZ EYLUL UNIVERSITY SCHOOL OF MARITIME BUSINESS AND MANAGEMENT DEPARTMENT OF DECK S elçuk N as SELÇUK NAS
DOKUZ EYLUL UNIVERSITY SCHOOL OF MARITIME BUSINESS AND MANAGEMENT DEPARTMENT OF DECK S elçuk N as SELÇUK NAS Declination of The Moon Large High Tide Small High Tide X Y
DOKUZ EYLUL UNIVERSITY SCHOOL OF MARITIME BUSINESS AND MANAGEMENT DEPARTMENT OF DECK S elçuk N as SELÇUK NAS Lowest Astronomical TideLAT Highest Astronomical TideHAT Mean Low WaterMLW Mean High WaterMHW Mean Low Water SpringsMLWS Mean High Water SpringsMHWS Mean Low Water NeapsMLWN Mean High Water NeapsMHWN Mean Lower Low WaterMLLW Mean Higher High WaterMHHW Mean Higher Low WaterMHLW Mean Lower High WaterMLHW Spring tideSp Neap tideNp
DOKUZ EYLUL UNIVERSITY SCHOOL OF MARITIME BUSINESS AND MANAGEMENT DEPARTMENT OF DECK S elçuk N as SELÇUK NAS BOTTOM CHARTED DEPTH MHWS CHART ELEVATION WATER LEVEL AIR DRAFT DRAFT MHWN MHWS MLWS MLWN CHART DATUM ( LATW ) High of Tide (HOT) DOKUZ EYLUL UNIVERSITY SCHOOL OF MARITIME BUSINESS AND MANAGEMENT DEPARTMENT OF DECK S elçuk N as SELÇUK NAS *1 : Please check the tide information of the charts for reference of elevation
DOKUZ EYLUL UNIVERSITY SCHOOL OF MARITIME BUSINESS AND MANAGEMENT DEPARTMENT OF DECK S elçuk N as SELÇUK NAS BA TIDE TABLE
DOKUZ EYLUL UNIVERSITY SCHOOL OF MARITIME BUSINESS AND MANAGEMENT DEPARTMENT OF DECK S elçuk N as SELÇUK NAS BA TIDE TABLE
DOKUZ EYLUL UNIVERSITY SCHOOL OF MARITIME BUSINESS AND MANAGEMENT DEPARTMENT OF DECK S elçuk N as SELÇUK NAS
DOKUZ EYLUL UNIVERSITY SCHOOL OF MARITIME BUSINESS AND MANAGEMENT DEPARTMENT OF DECK S elçuk N as SELÇUK NAS THIS PRESENTATION WAS PREPARED BY SELÇUK NAS E MAIL : Mobile Phone : Phone : Adress : Dokuz Eylul Universitesi, Deniz İsletmeciligi ve Yonetimi Yuksekokulu, Kaynaklar Yerleskesi, Buca, Izmir, TURKEY