Summertime increases in upper-ocean stratification and mixed-layer depth
The surface mixed layer of the world ocean regulates global climate by controlling heat and
carbon exchange between the atmosphere and the oceanic interior,–. The mixed layer also …
carbon exchange between the atmosphere and the oceanic interior,–. The mixed layer also …
Seasonal to decadal predictions with MIROC6: Description and basic evaluation
T Kataoka, H Tatebe, H Koyama… - Journal of Advances …, 2020 - Wiley Online Library
The present paper presents results of seasonal‐to‐decadal climate predictions based on a
coupled climate model called the Model for Interdisciplinary Research on Climate version 6 …
coupled climate model called the Model for Interdisciplinary Research on Climate version 6 …
Imprints of Atlantic Multidecadal Oscillation on pantropical seawater pH inferred from coral δ11B records
Understanding natural variability in seawater pH (pH sw) is crucial for predicting future
ocean acidification. Coral boron isotopes (δ 11 B) offer an alternative method to extend pH …
ocean acidification. Coral boron isotopes (δ 11 B) offer an alternative method to extend pH …
Revisiting the tropical atlantic influence on El Niño–Southern oscillation
The influence of the tropical Atlantic on El Niño–Southern Oscillation (ENSO) is examined
using sensitivity experiments with the SINTEX-F general circulation model with prescribed …
using sensitivity experiments with the SINTEX-F general circulation model with prescribed …
Observed relative contributions of anomalous heat fluxes and effective heat capacity to sea surface temperature variability
Sea surface temperatures (SSTs) vary not only due to heat exchange across the air‐sea
interface but also due to changes in effective heat capacity as primarily determined by mixed …
interface but also due to changes in effective heat capacity as primarily determined by mixed …
The Atlantic meridional mode and associated wind–SST relationship in the CMIP6 models
F Xia, J Zuo, C Sun, A Liu - Atmosphere, 2023 - mdpi.com
The Atlantic Meridional Mode (AMM) is the dominant mode of interannual climate variability
in the tropical Atlantic, maintained primarily by the positive wind–evaporation–sea surface …
in the tropical Atlantic, maintained primarily by the positive wind–evaporation–sea surface …
A simple coupled model of the wind–evaporation–SST feedback with a role for stability
KB Karnauskas - Journal of Climate, 2022 - journals.ametsoc.org
The wind–evaporation–SST (WES) feedback describes a coupled mechanism by which an
anomalous meridional sea surface temperature (SST) gradient in the tropics evolves over …
anomalous meridional sea surface temperature (SST) gradient in the tropics evolves over …
Mixed layer deepening due to wind-induced shear-driven turbulence and scaling of the deepening rate in the stratified ocean
Y Ushijima, Y Yoshikawa - Ocean Dynamics, 2020 - Springer
Wind-induced mixing forms the surface mixed layer (ML) above the stratified interior oceans.
The ML depth (MLD), a key quantity for several upper ocean processes such as the air-sea …
The ML depth (MLD), a key quantity for several upper ocean processes such as the air-sea …
Rainfall–Mixed Layer–SST Feedback Contributing to Atlantic Meridional Mode Development
T Kataoka, T Suzuki, H Tatebe - Journal of Climate, 2023 - journals.ametsoc.org
A simple air–sea coupled model for wind–evaporation–sea surface temperature (SST), wind-
induced turbulence–mixed layer (ML)–SST, and wind–evaporation–ML–SST feedback is …
induced turbulence–mixed layer (ML)–SST, and wind–evaporation–ML–SST feedback is …
Causal relationship between sea surface temperature and precipitation revealed by information flow
Z Ye, T Tozuka - Frontiers in Climate, 2022 - frontiersin.org
The atmosphere and the ocean are coupled with each other through various processes.
Therefore, it is of great importance to understand the causality relationship between the …
Therefore, it is of great importance to understand the causality relationship between the …