由于脱而导致的北极臭氧损失
1Max-Planck-Institut fur Chemie, Post Office Box 3060, 55020 Mainz, Germany. Forschungszentrum Karlsruhe, Institut fur Meteorologie und Klimaforschung, Post Office Box 3640, D-76021 Karlsruhe, Germany. FU Berlin, Institut fur Meteorologie, Carl-Heinr.
概括
由酸三水化合物颗粒驱动的北极脱,显著增加了臭氧层的损耗. 未来的平流层冷却可能会推迟臭氧的恢复,直到21世纪末.
科学领域:
- 大气化学 大气化学
- 石流层科学 石流层科学
- 气候建模气候模型
背景情况:
- 北极臭氧层的损耗是一个重大的环境问题.
- 平流层的活性在臭氧化学中起着至关重要的作用.
- 颗粒沉是平流层中已知的过程.
研究的目的:
- 调查粒子沉积在北极脱过程中的作用.
- 量化脱化对北极臭氧损失的影响.
- 评估北极臭氧恢复的未来轨迹.
主要方法:
- 用1994-95年的观测数据限制一个微物理模型.
- 模拟脱过程及其对臭氧的影响.
- 对平流层条件进行敏感性研究.
主要成果:
- 脱主要是由低密度的酸三水合物颗粒引起的.
- 脱化大大增加了北极的臭氧损失.
- 北极的平流层接近一个脱门.
结论:
- 人为二氧化碳的增加可能导致平流层的冷却.
- 未来的冷却可能会增强脱.
- 预计北极臭氧的恢复将被推迟到21世纪末.
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