An interaction network perspective on the relation between patterns of sea surface temperature variability and global mean surface temperature [PDF]
On interannual- to multidecadal timescales variability in sea surface temperature appears to be organized in large-scale spatiotemporal patterns. In this paper, we investigate these patterns by studying the community structure of interaction networks ...
A. Tantet, H. A. Dijkstra
doaj +1 more source
Sources of Uncertainty in Ocean Net Primary Productivity Projections Under Climate Change
Abstract The divergent representation of ocean net primary productivity (NPP) in Earth system models (ESMs) causes uncertainty in NPP projections, which must be reduced to effectively inform marine management and climate mitigation strategies. Here, we investigate the sources of uncertainty in monthly‐mean NPP by seven ESMs under four emissions ...
Natacha Le Grix, Alessandro Tagliabue
wiley +1 more source
The North Atlantic sea surface temperature exhibits fluctuations on the multidecadal time scale, a phenomenon known as the Atlantic Multidecadal Oscillation (AMO).
Yannick Peings, Gudrun Magnusdottir
doaj +1 more source
Reproduction of Twentieth Century Intradecadal to Multidecadal Surface Temperature Variability in Radiatively Forced Coupled Climate Models [PDF]
[1] Coupled Model Intercomparison Project 3 simulations that included time-varying radiative forcings were ranked according to their ability to consistently reproduce twentieth century intradecadal to multidecadal (IMD) surface temperature variability at
Boer +40 more
core +2 more sources
East Asian synoptic climatology linked to Atlantic multidecadal variability
The Atlantic Multidecadal Oscillation (AMO) is a climate phenomenon that can be observed in historical data and has potential connections to global synoptic climatic changes. The AMO can be used to predict climate patterns. This study examined how AMO-induced changes in the westerly jet stream over East Asia could affect the climatological distribution
Chi-Hua Wu, Pei-Chia Tsai
openaire +2 more sources
Abstract Satellite observations since 2001 show an increasing Earth's energy imbalance (EEI) at the top of the atmosphere of 0.45 W m−2 dec−1, a trend understated in coupled climate models. We assess the 2001–2024 EEI trend in historical simulations of two high‐resolution coupled models, CM4X, a revised version of CM4.0, and CESM‐HR, a high‐resolution ...
Yan‐Ting Chen +7 more
wiley +1 more source
Is there evidence of changes in tropical Atlantic variability modes under AMO phases in the observational record? [PDF]
The Atlantic multidecadal oscillation (AMO) is the leading mode of Atlantic sea surface temperature (SST) variability at multidecadal time scales. Previous studies have shown that the AMO could modulate El Niño–Southern Oscillation (ENSO) variance ...
Alban Lazar +8 more
core +3 more sources
North Atlantic Multidecadal SST Oscillation: External forcing versus internal variability
Abstract The Atlantic Multi-decadal Oscillation (AMO) depicts the swings of North Atlantic basin-wide sea surface temperature (SST) between warm and cold phases on a multi-decadal time scale. The 20th Century instrumental record indicates a relative cold period in the beginning of the 20th Century, a warm period in the 1940s and 50s, another cold ...
Ting, Mingfang +2 more
openaire +3 more sources
Abstract The Atlantic Meridional Overturning Circulation (AMOC) is a key regulator of the Earth's climate. Here using water hosing experiments with a coupled climate model, we show that a weakened AMOC leads to a significant boreal winter upper troposphere/lower stratosphere (UTLS) warming over the extratropical North Pacific (ENP).
Rajat Joshi, Rong Zhang
wiley +1 more source
Multidecadal Variations in the Tropical Western Pacific Driven by Externally‐Forced AMV‐Like Changes
Multidecadal sea surface temperature (SST) variations in the tropical western Pacific (TWP) have been attributed to nonlinear external forcing and remote influences from the Atlantic Multidecadal Variability (AMV).
Minhua Qin +3 more
doaj +1 more source

