Tides and solar radiation were included, except for tides in the Baltic Sea where they are negligible.
The physical processes at work include solar radiation, wind forcing, river discharge, tides, and water exchange with adjacent seas.
The Sun's energy flows through the earth system and out the other side, ebbing back into the coldness of space as a tide of infrared radiation.
The model used here to describe the rigid-body spacecraft dynamics includes the non-uniform rotating gravity field of the small body up to second degree and order along with the attitude dependent terms, solar tide, and solar radiation pressure.
Other factors linked to coral bleaching include rising acidity associated with the increased absorption of carbon dioxide by the oceans, ultraviolet radiation exposure, drying from extreme low-tide events (such as those associated with El Niño), sedimentation, pollution, and disease.
Migrating tides are predominantly forced by solar radiation absorption in tropospheric water vapor and stratospheric ozone.
At 110 km and equatorward of about 50°, the tidal fields that have propagated vertically from lower atmosphere sources dominate over those tides excited in situ from EUV solar radiation absorption ([Forbes and Garrett 1979]).
Many of these areas with high seawater temperatures also have a wide tidal range, and shellfish in these locations are exposed to solar radiation in intertidal dry beds at ebb and low tides and can reach temperatures of 30°C.
In the lower atmosphere, a dominant ISO is observed in the period band approximately 30 to 60 days in the outgoing longwave radiation (OLR) (a proxy for convection), total columnar water vapor (a proxy for tides), and zonal wind.
The diurnal tide anomalies over the two stations are correlated with the outgoing longwave radiation anomalies over the western Pacific region (120°E).
