Our seasonal cycle analysis further reveals clear differences in temporal trends among vegetation types: Dense Ombrophilous Forest exhibited an increase of ~ 0.099 ppm yr −1 , whereas Open Ombrophilous Forest showed a negative trend of ~−0.040 ppm yr −1 .
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Predominantly positive XCO<sub>2</sub> anomalies in the Caatinga biome highlight carbon vulnerability.
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