在过去的两千年里,甲来源的自然和人为变化
C J Sapart1, G Monteil, M Prokopiou
1Institute for Marine and Atmospheric Research Utrecht, Utrecht University, Princetonplein 5, 3584CC Utrecht, The Netherlands. c.j.sapart@uu.nl
Nature
|October 6, 2012
概括
格陵兰岛的冰芯揭示了过去的甲变化是由自然气候变化和人类活动驱动的. 同位素分析有助于确定过去2000年的这些来源.
科学领域:
- 古气候学 古气候学
- 大气化学 大气化学
- 同位素地球化学 同位素地球化学
背景情况:
- 甲 (CH4) 是一种强大的温室气体,具有多种自然和人为来源.
- 了解过去的大气甲变化对于气候建模至关重要.
- 甲来源的同位素签名提供了一种方法来追踪其起源.
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