Deep currents construct a circulation that spans
the whole global ocean. They play an active role in the
Earth's climate system, for example, during glaciations, and
they moderate anthropogenic climate change. Deep currents
influence climate by sequestering and transporting heat, salt,
and carbon around the planet. Yet compared to surface
currents, which can be observed from space, they remain
mysterious. This talk will discuss aspects of the deep
circulation in the North Atlantic and Arctic Oceans. The deep
currents in this region are part of the Atlantic Meridional
Overturning Circulation (AMOC), which is implicated in past
climate fluctuations and future climate change. Modern coupled
climate models used for climate projections fail to capture
some essential processes controlling the AMOC in the North
Atlantic and Arctic Oceans. Overflows through topographic
gaps, like between Greenland and Iceland, are an example. The
overflows involve mixing during intense events that last
O(1-10) hours. The mixing transforms the deep water
properties, which are then maintained by the deep flow for
O(10-100)years across planetary distances. This wide
separation of scales poses serious challenges to observing or
modeling deep currents. Yet modern ultra-high-resolution
regional ocean circulation models are increasingly realistic
and revealing of these flows.
About the Speaker:
Tom Haine is a Professor in the department
of Earth & Planetary Sciences at Johns Hopkins University.
His training is in physics and oceanography. He studies and
teaches ocean circulation and dynamics, and the ocean's role
in Earth's climate. Particular interests are the North
Atlantic and Arctic Oceans, and their rotating-stratified
fluid dynamics, which are exquisite. His approaches are
computational and theoretical, although he collaborates with
observational oceanographers and has participated in twelve
research expeditions. In 2019 he co-authored (with Barry
Klinger) a graduate level textbook, entitled Ocean Circulation
in Three Dimensions (Cambridge University Press).