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Advances in meson spectroscopy can enhance our understanding of how composite objects emerge from the fundamental underlying theory of interacting quarks and gluons, quantum chromodynamics.
Palaeoclimatic evidence of monsoon rainfall dynamics across different regions and timescales suggests that monsoon systems exhibit substantial regional variation; meridional temperature gradients are a major driver of monsoon variability, but these gradients are influenced by other, interacting forcing mechanisms, making predictions of future changes in monsoon rainfall highly uncertain.