Data for: Water and sediment temperature dynamics in shallow tidal environments: the role of the heat flux at the soil-water interface.

Water and sediment temperature data collected in a shallow tidal flat located in the Northern part of the Venice lagoon (see figure 1 in the manuscript).
The bottom elevation at the measuring station is 0:65 m below mean sea level, and the local tidal range is about 0.80 m during a spring tide and 0.50 m during a neap tide.
5 sensors (ControlByWeb, Xytronix Inc. Utah, USA) were deployed in the sediment (depth of 5, 25, 50, 100, and 150 cm below the sediment surface) and 4 sensors in the water column (10, 40, 70, 100 cm above the sediment surface). Data were collected with a 5 minutes resolution.

本数据集采集自威尼斯潟湖北部一处浅潮滩的水体与沉积物温度数据（详见手稿中的图1）。
该监测站的底床高程低于平均海平面0.65米，当地大潮潮差约为0.80米，小潮潮差约为0.50米。
共部署9台传感器：其中5台为ControlByWeb（美国犹他州Xytronix公司）设备，布设于沉积物中，布设深度分别为沉积物表层以下5、25、50、100及150厘米；另外4台布设于水柱中，布设高度为沉积物表层以上10、40、70及100厘米。所有数据的采集分辨率为5分钟。