348
V. Barale and M. Gade
Fig. 17.6 Red Sea ws [m s
−1 ] climatological monthly means (QuikSCAT data set)
Most chl values remain low, in particular for the basin interior, from May to
June, until the same summer spatial distribution seen at the beginning of this seasonal sequence is reached once again. Similarly, the prevailing swinds continue to
V. Barale and M. Gade
Fig. 17.6 Red Sea ws [m s
−1 ] climatological monthly means (QuikSCAT data set)
Most chl values remain low, in particular for the basin interior, from May to
June, until the same summer spatial distribution seen at the beginning of this seasonal sequence is reached once again. Similarly, the prevailing swinds continue to
