How do satellites “see” wind?
Satellites estimate winds by tracking the motion of clouds (or water vapor features in the absence of clouds) from a sequence of satellite images. Low Earth-orbiting satellites that circle the Earth from pole to pole around 600 miles up are typically used to understand wind patterns over Earth’s polar regions. Geostationary satellites, like GOES-16 and GOES-17, that stay in place above a set area by orbiting in tandem with the Earth as it turns, provide an almost constant stream of images of a given area, such as the United States. Frequent imaging is especially useful when tracking clouds because they often change shape as they evolve or dissipate. This frequent imaging allows for nearly continuous generation of wind estimates.
What is “wind shear” and how does it lead to thunderstorms?
Vertical wind shear, the change in wind's direction and speed with height, is a critical factor in determining whether severe thunderstorms will develop.
In this image, the thunderstorm on the left has a weakly sheared environment, while the one on the right is in a strongly sheared environment. The storm experiencing little or no wind shear will produce a vertical updraft, and the storm will be short-lived. On the other hand, the storm experiencing strong wind shear will develop a tilted updraft with the rain falling away from the updraft, helping to sustain the storm.
Improved Technology Leads to Better Wind-Monitoring
With advances in satellite technology, forecasters and climate scientists can utilize near real-time imagery and measurements of wind speeds across multiple levels of the atmosphere like never before.
“Being able to get reliable wind data remotely from satellites helps our meteorologists provide better forecasts and warnings,” explained meteorologist Brian Jackson from the National Weather Service. “Plus, satellite-derived wind data are especially important in areas where direct observations are unavailable, like sparsely populated locations, as well as over the ocean.”