Bagnell A, DeVries T
Interdepartmental Graduate Program in Marine Science, University of California, Santa Barbara, USA.
Department of Geography, University of California, Santa Barbara, USA.
Nat Commun. 2021 Jul 29;12(1):4604. doi: 10.1038/s41467-021-24472-3.
The historical evolution of Earth's energy imbalance can be quantified by changes in the global ocean heat content. However, historical reconstructions of ocean heat content often neglect a large volume of the deep ocean, due to sparse observations of ocean temperatures below 2000 m. Here, we provide a global reconstruction of historical changes in full-depth ocean heat content based on interpolated subsurface temperature data using an autoregressive artificial neural network, providing estimates of total ocean warming for the period 1946-2019. We find that cooling of the deep ocean and a small heat gain in the upper ocean led to no robust trend in global ocean heat content from 1960-1990, implying a roughly balanced Earth energy budget within -0.16 to 0.06 W m over most of the latter half of the 20th century. However, the past three decades have seen a rapid acceleration in ocean warming, with the entire ocean warming from top to bottom at a rate of 0.63 ± 0.13 W m. These results suggest a delayed onset of a positive Earth energy imbalance relative to previous estimates, although large uncertainties remain.
地球能量失衡的历史演变可以通过全球海洋热含量的变化来量化。然而,由于对2000米以下海洋温度的观测稀少,海洋热含量的历史重建往往忽略了大量的深海区域。在此,我们基于使用自回归人工神经网络的插值次表层温度数据,对全深度海洋热含量的历史变化进行了全球重建,给出了1946 - 2019年期间海洋总变暖的估计值。我们发现,1960 - 1990年期间,深海冷却以及上层海洋少量的热量增加导致全球海洋热含量没有明显趋势,这意味着在20世纪后半叶的大部分时间里,地球能量收支大致平衡在-0.16至0.06瓦每平方米之间。然而,在过去三十年中,海洋变暖迅速加速,整个海洋从表层到深层以0.63±0.13瓦每平方米的速率变暖。这些结果表明,相对于先前的估计,地球正能量失衡的开始有所延迟,尽管仍然存在很大的不确定性。