The Importance of Incorporating Diurnally Fluctuating Stream Discharge in Stream Temperature Energy Balance Models

HFLUX input data used to run the diurnally fluctuating streamflow base case model discussed in Baker et al. (2018), "The Importance of Incorporating Diurnally Fluctuating Stream Discharge in Energy Balance Models to Determine Groundwater Inflow Rates". The HFLUX model can be downloaded from http://hydrology.syr.edu/hflux/, where additional information on the model structure and inputs is located. The 18 excel sheets include the model settings, time steps, distance steps, temperature boundary conditions in space and time, stream channel geometry, discharge data, groundwater temperatures averaged from 5 wells, weather data, average stream bed temperatures and the depth at which they were measured, sediment time, shade and cloud data, site latitude, longitude, and elevation, and the calibrated stream temperatures through space and time over a ~1.2 km reach over a ~5 day period.

This resource will be made public/published upon the acceptance of the corresponding manuscript.

HFLUX 输入数据集，用于运行 Baker 等人于 2018 年发表的论文中讨论的日波动河流流量基础模型，即《在确定地下水补给速率的平衡模型中纳入日波动河流流量的重要性》。HFLUX 模型可从 http://hydrology.syr.edu/hflux/ 下载，该网址提供了模型结构和输入参数的附加信息。该数据集包含 18 个 Excel 工作表，涵盖了模型设置、时间步长、距离步长、空间和时间边界条件下的温度、河流渠道几何形状、流量数据、由 5 个井平均得到的地下水温度、气象数据、平均河床温度及其测量深度、沉积物时间、阴影和云数据、场地纬度、经度和高程，以及在一个约 1.2 公里长的河段上，约 5 天时间内空间和时间上的校准河流温度。该资源将在相应论文被接受后公开/发布。