Evidence from dryland and arid region studies confirms that desert areas actively influence regional hydrological cycles and local climates through soil moisture, vegetation feedbacks, and drought dynamics.
The claim states that desert areas significantly influence and modify local climates. Papers 1 and 6 provide direct evidence of feedback mechanisms—such as soil moisture-precipitation interactions and vegetation-drought feedbacks in arid basins—demonstrating that dryland areas actively shape regional climates. Other papers discuss arid land dynamics and climate interactions, aligning with the supportive evidence.