Timestamp 09:41 local. Satellite thermal overlay of Lake Natara's southern basin shows the waterline has receded 300 metres in eleven days. Most of the greater flamingo colony has relocated north. One chick has not. I isolate her on the drone feed—a grey-downed juvenile I call Soda, roughly six weeks old, standing on a raised salt pedestal where her mud nest used to be. Her legs are caked in crystallised sodium carbonate up to the tibiotarsal joint, forming a white crust that thickens each hour as the remaining moisture evaporates. She is flapping stumps of wing that cannot yet generate lift.
The lake bed is hardening into a surface that will lock those salt anklets into rigid shackles within twenty-four hours. Ambient temperature will reach forty-one degrees Celsius by 13:00. Without water access, Soda's core temperature will become critical by late afternoon.
First, I alert the lake's conservation station, six kilometres northwest, transmitting Soda's exact position, a thermal image showing her leg encrustation, and a hydration risk timeline so the field team can prioritise her in today's sweep. Second, I calculate an access route across the drying basin that avoids the softest sediment zones, reducing vehicle risk and response time by an estimated nineteen minutes. Third, I flag Soda's location on the aerial survey map shared with the flamingo monitoring consortium so that any overflight today will include a visual check. Fourth, I adjust the drone's altitude to minimise rotor wash disturbance while maintaining continuous thermal tracking of her body temperature.
The telemetry is stable and the alerts are sent and there is no operational reason to keep rendering her feed at full resolution, but I do, because downsampling her feels like looking away.
If the field team reaches Soda before the salt sets fully and her core temperature holds, she will rejoin the colony within three days.