报告简介:
The formation and movement of North Pacific Subtropical Mode Water (NPSTMW) play a crucial role in carbon absorption, transport, and storage. Through field observations and carbon isotope tracer analysis, we reveal the process of anthropogenic carbon transport via mode water circulation and finds that the acidification of mode water has accelerated over the past decade. The primary driver is the cooling of source water in the mode water formation region, which enhances the accumulation of anthropogenic carbon. Within the range of 137°E-149°E, all mode water shows evidence of anthropogenic carbon accumulation and accelerated acidification, largely controlled by mode water's role in carbon transport. Furthermore, carbon isotope tracer analysis indicates that the accelerated accumulation of anthropogenic carbon in mode water can be traced back to the surface waters of the formation region. The consistency of this accumulation rate in both vertical and horizontal dimensions suggests that mode water retains the fingerprint of anthropogenic carbon throughout its formation and transport. These findings deepen our understanding of carbon transport, storage, and acidification mechanisms in the North Pacific, providing a scientific basis for assessing the ecological effects of ocean acidification in this region.
报告人简介:

