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热带和极地温度同步演变
Marlow J Cramwinckel1, Matthew Huber2, Ilja J Kocken3
1Department of Earth Sciences, Faculty of Geoscience, Utrecht University, Utrecht, The Netherlands. m.j.cramwinckel@uu.nl.
Nature
|July 4, 2018
概括
重建具有高大气二氧化碳 (CO2) 气候有助于预测未来的气候变化. 这项研究揭示了热带和深海温度的平行变化,
科学领域:
- 古气候学
- 气候模型
- 地质化学
背景情况:
- 对于未来的气候变化预测,了解过去高二氧化碳的温暖气候至关重要.
- 纪 (56-3400万年前) 是6600万年来最热的时期,但连续热带气温数据很少.
- 之前的研究证实了以纪的极地温暖,强调了需要热带温度记录来量化全球气候演变的必要性.
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