Bjerknes Compensation in Meridional Heat Transport under Freshwater Forcing and the Role of Climate Feedback

Using a coupled Earth climate model, freshwater forcing experiments are performed to study the Bjerknes compensation (BJC) between meridional atmosphere heat transport (AHT) and meridional ocean heat transport (OHT). Freshwater hosing in the North Atlantic weakens the Atlantic meridional overturning...

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Bibliographic Details
Published in:Journal of Climate
Main Authors: Yang, Haijun, Wen, Qin, Yao, Jie, Wang, Yuxing
Other Authors: Yang, HJ (reprint author), Peking Univ, Sch Phys, Lab Climate & Ocean Atmosphere Studies, Beijing, Peoples R China.; Yang, HJ (reprint author), Peking Univ, Sch Phys, Dept Atmospher & Ocean Sci, Beijing, Peoples R China., Peking Univ, Sch Phys, Lab Climate & Ocean Atmosphere Studies, Beijing, Peoples R China., Peking Univ, Sch Phys, Dept Atmospher & Ocean Sci, Beijing, Peoples R China., State Oceanol Adm, Natl Marine Environm Forecasting Ctr, Beijing, Peoples R China., Yang, HJ (reprint author), Peking Univ, Sch Phys, Dept Atmospher & Ocean Sci, Beijing, Peoples R China.
Format: Journal/Newspaper
Language:English
Published: JOURNAL OF CLIMATE 2017
Subjects:
NORTH-ATLANTIC OCEAN
THERMOHALINE CIRCULATION
ENERGY TRANSPORTS
TROPICAL OCEAN
ATMOSPHERE
MODEL
VARIABILITY
AQUAPLANET
CCSM4
FLUX
Pacific
North Atlantic
Online Access:https://hdl.handle.net/20.500.11897/472494
https://doi.org/10.1175/JCLI-D-16-0824.1
Description
Summary:Using a coupled Earth climate model, freshwater forcing experiments are performed to study the Bjerknes compensation (BJC) between meridional atmosphere heat transport (AHT) and meridional ocean heat transport (OHT). Freshwater hosing in the North Atlantic weakens the Atlantic meridional overturning circulation (AMOC) and thus reduces the northward OHT in the Atlantic significantly, leading to a cooling (warming) in the surface layer in the Northern (Southern) Hemisphere. This results in an enhanced Hadley cell and northward AHT. Meanwhile, the OHT in the Indo-Pacific is increased in response to the Hadley cell change, partially offsetting the reduced OHT in the Atlantic. Two compensations occur here: compensation between the AHT and the Atlantic OHT, and that between the Indo-Pacific OHT and the Atlantic OHT. The AHT change undercompensates the OHT change by about 60% in the extratropics, while the former overcompensates the latter by about 30% in the tropics due to the Indo-Pacific change. The BJC can be understood from the viewpoint of large-scale circulation change. However, the intrinsic mechanism of BJC is related to the climate feedback of the Earth system. The authors' coupled model experiments confirm that the occurrence of BJC is an intrinsic requirement of local energy balance, and local climate feedback determines the extent of BJC, consistent with previous theoretical results. Even during the transient period of climate change, the BJC is well established when the ocean heat storage is slowly varying and its change is much weaker than the net local heat flux change at the ocean surface. The BJC can be deduced from the local climate feedback. Under the freshwater forcing, the overcompensation in the tropics is mainly caused by the positive longwave feedback related to clouds, and the undercompensation in the extratropics is due to the negative longwave feedback related to surface temperature change. Different dominant feedbacks determine different BJC scenarios in different regions, which are in essence constrained by local energy balance. NSF of China [41376007, 41176002, 91337106] SCI(E) ARTICLE 14 5167-5185 30

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