. Calculation of hydrographic position data by least squares Oceanography. where D = t^i -q«)*+ 4 =|3 /« (H-7J 4. If the positive value of D satisfying eq. (H-7) is choosen, then the semi-major axis of the error ellipse is positioned along the "new" x-axis. Therefore, from the a two solutions C^ = d. and 0^ - o<-+90 satisfying eq. (H-4) the valid one must be choosen (considering o( as the smallest positive angle satisfying (H-4)).. FIG H-2: ERROR ELLIPSE The only way to solve that ambiguity is to test either with 0(1 or o<2- For that purpose, it is recommended to a
. Calculation of hydrographic position data by least squares Oceanography. where D = t^i -q«)*+ 4 =|3 /« (H-7J 4. If the positive value of D satisfying eq. (H-7) is choosen, then the semi-major axis of the error ellipse is positioned along the "new" x-axis. Therefore, from the a two solutions C^ = d. and 0^ - o<-+90 satisfying eq. (H-4) the valid one must be choosen (considering o( as the smallest positive angle satisfying (H-4)).. FIG H-2: ERROR ELLIPSE The only way to solve that ambiguity is to test either with 0(1 or o<2- For that purpose, it is recommended to a) obtain the point of intersection (either P, or t\ ) 124. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Silva, Francisco Castro e. ;Castro e Silva,
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Keywords: ., bookcentury1900, bookcollectionamerican, booksubjectoceanography
