Globally, thermodynamics explains an increase in atmospheric water vapor with warming of
around 7%/° C near to the surface. In contrast, global precipitation and evaporation are …

This chapter assesses simulations of future global climate change, spanning time horizons
from the near term (2021–2040), mid-term (2041–2060), and long term (2081–2100) out to …

Understanding Future Change of Global Monsoons Projected by CMIP6 Models in: Journal of
Climate Volume 33 Issue 15 (2020) Jump to Content Jump to Main Navigation Logo Logo Logo …

Monsoon rainfall has profound economic and societal impacts for more than two-thirds of the
global population. Here we provide a review on past monsoon changes and their primary …

Abstract Changes in global land monsoon (GLM) precipitation determine the local water
resource, affecting two thirds of global population. The future changes in GLM summer …

Abstract The Afro-Asian summer monsoon (AfroASM) sustains billions of people living in
many developing countries covering West Africa and Asia, vulnerable to climate change …

An accurate prediction of land monsoon precipitation (LMP) is critical for the sustainable
future of the planet as it provides water resources for more than two-thirds of the global …

Coupled climate system models consistently show that the low-level southerly wind
associated with the East Asian summer monsoon (EASM) is enhanced under anthropogenic …

The anthropogenic warming of the Earth's atmosphere is causing dynamical and
thermodynamical changes in the ocean and atmosphere circulation, including the Asian …

Despite a globally uniform increase in the concentrations of emitted greenhouse gases,
radiatively forced surface warming can have significant spatial variations. These define …