{ } JustinGeoSci

Thermal Sciences

Near-surface atmospheric physics, from energy balance to human heat exposure.

The near-surface atmosphere is where incoming solar energy is absorbed, re-radiated, and traded with the ground through turbulence and evaporation; that balance sets the surface temperature and the daily cycle of heat and moisture. Describing it means a connected chain of calculations: the state of the air (temperature, humidity, wind, pressure), the radiation that powers the exchange, the surface fluxes, and the energy balance that ties them together. A step further, the same conditions set the heat a person is subjected to outdoors, which thermal indices summarize.

Each package implements these relationships straight from their published sources, under one set of conventions: pressure in kilopascals, temperatures in the user’s chosen unit, and a single sign convention for the energy balance. Every function names the equation it uses and shows a worked example, and it accepts NumPy arrays as readily as single values.

Atmoflux is the foundation layer. The thermal indices that build on this atmospheric groundwork are in development and will join this area as they reach the same standard of documentation and testing.