SATELLITE ALTIMETRY AND TIDE GAUGE OBSERVATIONS BOTH HAVE THE TRACE OF OCEAN TIDE AND SO CAN BE USED TO DIAGNOSE AND RESOLVE TIDAL CONSTITUENTS. THE PRESENT PAPER APPLIES SOME PROCEDURES TO MAKE A COMBINED TIDAL MODEL. SEA SURFACE DATA FROM SATELLITE ALTIMETRY MISSIONS (TOPEX- POSEIDON, JASON 1 AND JASON 2) ALONG WITH NCC'S TIDE GAUGE DATA AND SOME SEA LEVEL DATA FROM UNIVERSITY OF HAWAII SEA LEVEL CENTER (UHSLC) IS USED IN THIS STUDY. THEREAFTER, TIME SERIES ARE PRODUCED AND ANALYZED USING LEAST SQUARE SPECTRAL ANALYSIS ((LSSA)) TECHNIQUE TO RECOVER EFFECTIVE FREQUENCIES. RESIDUALS ARE THEN USED FOR DATA CLEANING AND SO OUTLIERS ARE DETECTED AND ELIMINATED IMPLEMENTING A SIMPLE 3SIGMA TEST. THE EFFECT OF TEMPORAL ALIASING PHENOMENA ASSOCIATED WITH SATELLITE ALTIMETRY IS CONSIDERED AND THEN, CLASSICAL HARMONIC ANALYSIS METHOD IS USED FOR TIDAL ANALYSIS OF SATELLITE ALTIMETRY AND TIDE GAUGE TIME SERIES AND CONSEQUENTLY AMPLITUDE AND PHASE OF CONSTITUENTS IS ESTIMATED. THE NEW DERIVED MODEL TM-IR01 IS EVALUATED BY COMPARING TO TIDE GAUGE STATIONS AND GLOBAL TIDE MODELS. VALIDATING WITH TIDE GAUGE STATIONS RESULTED IN ROOT MEAN SQUARE ERROR AS FOLLOWS: FOR MAIN TIDAL FREQUENCIES M2 WITH 0.372 RMSE, S2 WITH 0.130 RMSE, AND K1 WITH 0.141 RMSE AND O1 WITH 0.084. VALIDATING WITH GLOBAL TIDE MODELS. FES2004, FES2012 AND TPXO7.2 IS THEN CONSIDERED. ROOT MEAN SQUARE ERROR BETWEEN TM-IR01 AND FES2004 ARE AS FOLLOWS: FOR MAIN TIDAL FREQUENCIES M2 WITH 0.231 RMSE, S2 WITH 0.087 RMSE, AND K1 WITH 0.027 RMSE AND O1 WITH 0.042. ABOVE VALUES FOR THE MODEL FES2012 IS THE SAME. ROOT MEAN SQUARE ERROR BETWEEN TM-IR01 AND TPXO7.2 ARE AS FOLLOWS: FOR MAIN TIDAL FREQUENCIES M2 WITH 0.234 RMSE, S2 WITH 0.085 RMSE, AND K1 WITH 0.018 RMSE AND O1 WITH 0.044.