A team of researchers from the Institute of Atmospheric Physics at the Chinese Academy of Sciences reconstructed these ancient conditions using advanced climate simulations. Their findings showed a troubling trend: intense warming expanded subtropical dry zones while shrinking tropical wet regions. This disruption was tied to a significant reduction in the seasonal shifts of the Intertropical Convergence Zone (ITCZ) - a critical band of heavy rainfall and cloud cover that migrates between hemispheres with seasonal changes.
"In the early Eocene, much warmer oceans made evaporation far more sensitive to wind speed," explained Dr. REN Zikun, the study's lead author. "This heightened sensitivity amplified wind-driven differences in surface evaporation between hemispheres, disrupting the balance with solar heating. The result was a reduced seasonal reach of the ITCZ and a contraction of tropical wet zones."
"The deep-time history of Earth provides critical evidence of how greenhouse gases reshape the global climate," said Prof. ZHOU Tianjun, the study's corresponding author. "While the Eocene's changes unfolded over millennia, human-driven warming could force these shifts at an unprecedented pace. This underscores the urgent need for mitigation efforts to limit greenhouse gas emissions."
Research Report:Enhanced "Wind-Evaporation Effect" Drove the "Deep-Tropical Contraction" in the Early Eocene
Related Links
Institute of Atmospheric Physics, Chinese Academy of Sciences
Earth Observation News - Suppiliers, Technology and Application
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