“…The atmospheric correction method used to generate such products used the blue and red bands to estimate aerosol contributions after assuming certain relationship between surface reflectance in these bands, and then interpolated to other bands (Kaufman et al, ). Although named as “land surface reflectance,” the data products (denoted as “R_Land” in this study) do have global coverage including estuarine and inland waters; therefore have been used to study water quality in estuaries and inland waters (Chen et al, ; Constantin et al, ; Doxaran et al, ; Hou et al, ; Olmanson et al, ; Park & Latrubesse, ; Pavelsky & Smith, ; Petus et al, ; Song et al, ; Tarrant et al, ; Wang et al, ; Wu et al, ). Indeed, although designed for land studies, compared with the MODIS ocean bands, MODIS land bands have higher spatial resolutions (250–500 m) and larger dynamic ranges (Hu et al, ), making them particularly useful for relatively small water bodies (Binding et al, ; Chen et al, ; Feng et al, ; Hu et al, ; Kahru et al, ; Kutser et al, ; Lahet & Stramski, ; Markham et al, ; Saldías et al, ).…”