Researchers find biases in warming patterns in climate models of monsoons

Are ‘corrections’ the answer? Avoiding the need for them might be better. The researchers observe that ‘the projected warming in response to greenhouse gases is too great’. This has been known for years but the penny of reliance on a certain climate theory has yet to drop, it seems.
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Climate projections are crucial for adaptation and mitigation planning says Eurekalert.

The output of the latest round of the Coupled Model Intercomparison Project, phase 6 (CMIP6) has been widely used in climate projections.

However, a subset of CMIP6 models is “too hot” and the projected warming in response to greenhouse gases is too great.

How to tackle the “hot model” problem at the regional scale had previously been unclear.

A research team from the Institute of Atmospheric Physics (IAP) of the Chinese Academy of Sciences (CAS) has revealed that the latest CMIP6 climate models tend to overestimate future Afro-Asian summer monsoon (AfroASM) rainfall and runoff due to present-day biases in warming patterns.

By constraining biases, however, the rainfall increase is 70% of the raw projection. The study was published in Nature Communications on May 10.

The AfroASM includes the West African monsoon, South Asian monsoon, and East Asian monsoon.

The research team identified the leading mode of variability among CMIP6 models in projecting future changes in AfroASM rainfall. They found that projection uncertainty was related to the bias in present-day interhemispheric thermal contrast (ITC).

Since large-scale monsoon circulation is driven by ITC due to moist static energy gradients, models with a larger ITC trend over the past thirty years tend to project more precipitation increases.

Since most CMIP6 models tend to overestimate present-day ITC trends, the team corrected the raw projection by designing an emergent constraint technique.

The increase in precipitation in the constrained projection is ~70% of the ensemble mean of the CMIP6 models. The area of land with a significant increase in precipitation is ~57% of the raw projection.

The research team further extended its analysis to runoff, which is a mirror of potential water availability. In the constrained projection, ~27% of land area in the AfroASM region will witness a significant increase in potential water availability, which is ~66% of the raw projection.

Regionally, the impact of the observational constraint is most pronounced in the West African monsoon region where the fraction of land area with increased water availability is ~55% of the raw projection.

This study provides a solution for tackling the “hot model” problem at regional scales. The emergent constraint technique reported in the study is based on the physical link between a modelled but observable variable in the present day and a projected variable in the future climate system.

Full article here.