Conflicting reconstructions of Holocene variability of the East Asian summer monsoon
(EASM) from speleothem versus other types of proxy records have yielded widely divergent …

Wildfires affect 40% of the earth's terrestrial biome, but much of our knowledge of wildfire
activity is limited to the satellite era. Improved understanding of past fires is necessary to …

Abstract The Pacific Walker circulation (PWC) has an outsized influence on weather and
climate worldwide. Yet the PWC response to external forcings is unclear,, with empirical data …

Speleothem oxygen isotopic (δ18O) records are used to reconstruct past hydroclimate yet
records from the same cave do not always replicate. We use a global database of …

Paleoclimatic records provide valuable information about Holocene climate, revealing
aspects of climate variability for a multitude of sites around the world. However, such data …

Our understanding of climate dynamics during millennial-scale events is incomplete,
partially due to the lack of their precise phase analyses under various boundary conditions …

Speleothems from cold high-elevation (and high-latitude) caves are sensitive
paleoenvironmental archives, because they form close to the freezing point of water, and …

Uncertainty about the influence of anthropogenic radiative forcing on the position and
strength of convective rainfall in the Intertropical Convergence Zone (ITCZ) inhibits our …

Palaeoclimate information on multiple climate variables at different spatiotemporal scales is
becoming increasingly important to understand environmental and societal responses to …

The response of the hydrological cycle to anthropogenic climate change, especially across
the tropical oceans, remains poorly understood due to the scarcity of long instrumental …