The Double-ITCZ Problem in IPCC AR4 Coupled GCMs: Ocean–Atmosphere Feedback Analysis
By Jialin Lin. 2007
632 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/5e8138a8cff8e61acf55c073fe128eaf521e8787
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In Atmospheric Science
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In Oceanography
Citations in the corpus
- Improved ensemble-mean forecasting of ENSO events by a zero-mean stochastic error model of an intermediate coupled model (2016, background): “In contrast, over the cold tongue, a positive feedback between the SST and cloud is visible (Lin 2007).”
- The Norwegian Earth System Model, NorESM1-M – Part 1: Description and basic evaluation of the physical climate (2013, background): “Figure 8 shows that a main feature of the tropical bias is related to the double Intertropical Convergence Zone (ITCZ) problem that has long been a common error among climate models (Lin, 2007).”
- Mapping China's freshwater fishes: diversity and biogeography (2014, background): “9 Giga tons of coal equivalent, according to China’s national mid- to long-term development plans, which is very close to the Intergovernmental Panel on Climate Change – Special Report on Emissions Scenarios (IPCC SRES) B2 scenario (mid-low emissions scenario) (Lin 2007; Wu et al. 2010).”
- Simulation of Present-Day and Twenty-First-Century Energy Budgets of the Southern Oceans (2010, background): “mon to coupled climate models is the tendency to have a double-ITCZ structure for annual mean conditions (Lin 2007), resulting from a spurious migration of the ocean ITCZs into the SH.”
- MJO Simulation Diagnostics (2009, background): “…are the confounding issues concerning the representation of the basic state, including a preference for overdoing the ''double ITCZ'' (Lin 2007), a poor mean rainfall structure in the Indian Ocean (Sperber and Annamalai 2008), equatorial surface westerly winds that are too weak or…”
- The double ITCZ bias in CMIP5 models: interaction between SST, large-scale circulation and precipitation (2015, background): “In fact, in the CMIP3 models the precipitation patterns follow the SST patterns too closely compared to observations, especially over the southeastern tropical Pacific (Lin 2007).”