Abstract

Annual cycle is fundamental in the East Asian monsoon (EAM) systems, profoundly governing the spatiotemporal distribution of the East Asian rainfall. The present study identified the dominant modes of the annual cycle in the East Asian rainfall based on the Fourier harmonic analysis and the Empirical Orthogonal Function (EOF) decomposition. We evaluated the performance of the first two leading modes (i.e., EOF-1 and EOF-2) in historical experiments (1979–2014) of the 21 released climate models of phase six of the Coupled Model Intercomparison Project (CMIP6). Comparing with the observation, although the CMIP6 models yield the essential fidelity, they still show considerable systematic biases in the amplitude and phase of the annual cycle, especially in east and south China. Most models exhibit substantial phase delays in the EOF-2 mode of the annual cycle. Some specific models (BCC-ESM1, CanESM5, and GFDL-CM4) exhibiting better performance could capture the observed annual cycle and the underlying physics in climatology and interannual variability. The limited fidelity of the EOF-2 mode of the EAM annual cycle primarily hinders the monsoon variability simulation and thus the reliable future projection. Therefore, the dominant modes of the EAM annual cycle act as the evaluate benchmark in the EAM modelling framework. Their improvement could be one possible bias correction strategy for decreasing the uncertainty in the CMIP6 simulation of the EAM.

Highlights

  • Asian monsoon precipitation feeds billions of people over the regions with the world’s most dense population [1]

  • The multistage evolution and annual cycle of rainfall over East Asia correspond with the surface boundary forcing (e.g., sea surface temperature (SST), snow cover, and soil moisture) and internal atmospheric variabilities in observations

  • It is foreseeable that annual cycle of the monsoon system links with complicated and various modelling factors, including the mean state and cycle of the sea surface temperature (SST), mid-latitude processes, physical parameterizations, dynamic core, among others

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Summary

Introduction

Asian monsoon precipitation feeds billions of people over the regions with the world’s most dense population [1]. Despite its extremely heterogeneous structure and diverse behavior, the remarkable annual cycle of the Asian monsoon depends on the large-scale underlying forcing and constraints, which provides higher predictability than the monsoon rainfall in a given period. The summer rainbands over the East Asian continent are associated with different steps of the monsoon cycle. They present the northward migration of the primary narrow rain belt from the south (pre-monsoon rain) to central (Meiyu/Baiu front) and to North China (the polar front) [26,27,28]. The CMIP3 ensembles cannot sufficiently capture the observed northward movement of the East Asian rainband, they exhibit a developing inter-model consensus on the timing of the rainy season [34].

CMIP6 Archive and Observation
Definition of the Annual Cycle
Simulation of the Annual Cycle Component of East Asian Rainfall
Modes of the Annual Cycle of East Asian Rainfall
Discussion
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