Wurl O, Bird K, Cunliffe M, Landing W M, Miller U, Mustaffa N I H, Ribas-Ribas M, Witte C, Zappa C J
Institute for Chemistry and Biology of the Marine Environment Carl von Ossietzky University Oldenburg Wilhelmshaven Germany.
Marine Biological Association of the United Kingdom Plymouth UK.
Geophys Res Lett. 2018 May 16;45(9):4230-4237. doi: 10.1029/2018GL077946. Epub 2018 May 12.
This paper describes high-resolution in situ observations of temperature and, for the first time, of salinity in the uppermost skin layer of the ocean, including the influence of large surface blooms of cyanobacteria on those skin properties. In the presence of the blooms, large anomalies of skin temperature and salinity of 0.95°C and -0.49 practical salinity unit were found, but a substantially cooler (-0.22°C) and saltier skin layer (0.19 practical salinity unit) was found in the absence of surface blooms. The results suggest that biologically controlled warming and inhibition of salinization of the ocean's surface occur. Less saline skin layers form during precipitation, but our observations also show that surface blooms of sp. inhibit evaporation decreasing the salinity at the ocean's surface. This study has important implications in the assessment of precipitation over the ocean using remotely sensed salinity, but also for a better understanding of heat exchange and the hydrologic cycle on a regional scale.
本文描述了对海洋最上层表层温度的高分辨率原位观测,并且首次观测了该表层的盐度,包括蓝细菌大量表面水华对这些表层特性的影响。在有水华存在的情况下,发现表层温度和盐度出现了0.95°C和-0.49实用盐度单位的大幅异常,但在没有表面水华的情况下,发现了明显更冷(-0.22°C)且更咸的表层(0.19实用盐度单位)。结果表明,海洋表面存在生物控制的变暖以及盐化抑制现象。降水期间会形成盐度较低的表层,但我们的观测还表明, 种的表面水华会抑制蒸发,从而降低海洋表面的盐度。这项研究对于利用遥感盐度评估海洋降水具有重要意义,同时对于更好地理解区域尺度上的热交换和水文循环也具有重要意义。