The Annual Cycle of the Energy Budget. Part II: Meridional Structures and Poleward Transports

By John T. Fasullo, Kevin E. Trenberth. 2008

187 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/a07ac831c713e674e59adb560302e126566bb806

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. David Ferreira
2. John Marshall
3. Tobias Bischoff
4. David McGee
5. Tapio Schneider
6. J. Kiehl
7. A. Donohoe
8. John T. Fasullo

In Global and Planetary Change

1. David Ferreira
2. John Marshall
3. A. Donohoe
4. John T. Fasullo
5. Kevin E. Trenberth
6. Valerio Lucarini
7. Tobias Bischoff
8. Tapio Schneider

Citations in the corpus

• Simulation of Present-Day and Twenty-First-Century Energy Budgets of the Southern Oceans (2010, methodology): “When the radiative imbalance at the TOA is converted to the required northward energy transport (Fasullo and Trenberth 2008b; Trenberth and Fasullo 2008) and compared with the CMIP3 model values, systematic biases in the total and both atmosphere and ocean are evident (Fig.”
• Predicting Climate Change Using Response Theory: Global Averages and Spatial Patterns (2015, background): “We remind that the ocean contributes to about 30% of the total meridional heat transport in the present climate [6, 74, 75].”
• EC-Earth V2.2: description and validation of a new seamless earth system prediction model (2012, methodology): “Results derived from the EC-Earth PD run are compared with ERA15 reanalysis data from Trenberth and Caron (2001) and estimates from Fasullo and Trenberth (2008) Xie and Arkin (1996).”
• Towards multi-resolution global climate modeling with ECHAM6–FESOM. Part I: model formulation and mean climate (2015, background): “5) PW found at the same latitudes (Fasullo and Trenberth 2008).”
• The CNRM-CM5.1 global climate model: description and basic evaluation (2013, background): “Figure 14 shows the latitudinal total heat transport for the global and Atlantic-only ocean for the two model versions together with NEMO-FOR, NEMO-VAR and an independent estimate from satellite and reanalysis products (Fasullo and Trenberth 2008, hereafter FT08).”
• Earth's Global Energy Budget (2009, methodology): “Satellite retrievals from the ERBE and the CERES (Wielicki et al. 1996) datasets are used (see Fasullo and Trenberth 2008a for details).”
• Energetic Constraints on the Position of the Intertropical Convergence Zone (2013, methodology): “(3) gives Estimating the different terms from annually and zon-ally averaged reanalysis data (Uppala et al. 2005) and using 20 W m 2 2 for the net energy input in the de-nominator (Fasullo and Trenberth 2008) gives d 5 6 8 for the present climate, consistent with observations.”
• The ocean’s role in setting the mean position of the Inter-Tropical Convergence Zone (2013, methodology): “We use long term climatologies of the TOA fluxes that are corrected for missing data as in Fasullo and Trenberth (2008a).”
• The Annual Cycle of the Energy Budget. Part I: Global Mean and Land–Ocean Exchanges (2008, background): “The likely uncertainties in OE, especially in the Southern Hemisphere (Fasullo and Trenberth 2008), can alter apparent trends if the ocean observing system changes, as it has in recent years with Argo floats (Gouretski and Koltermann 2007), and may be a source of the discrepancy between the OE…”