The demise of Lowland Classic Maya civilization during the Terminal Classic Period (~ 800
to 1000 CE) is a well-cited example of how past climate may have affected ancient societies …

Hydroclimate variability on multi-decadal timescales has been a prominent feature of the
circum-Caribbean region over the common era, with marked dry intervals noted in particular …

The relationship between climatic-environmental changes and its cultural implications in the
Northern Mesoamerican Frontier is poorly understood, because of the lack of high-resolution …

Classic Maya populations living in peri-urban states were highly dependent on seasonally
distributed rainfall for reliable surplus crop yields. Despite intense study of the potential …

Reconstructing hydroclimate over the Common Era is essential for understanding the
dominant mechanisms of precipitation change and improving climate model projections …

Many early Maya cities developed along the edges of large structural or karst depressions
(bajos). This topographic position aided growing populations to more effectively capture and …

Many Holocene hydroclimate records show rainfall changes that vary with local orbital
insolation. However, some tropical regions display rainfall evolution that differs from gradual …

The paleoclimatic record from Mexico and Central America, or Mesoamerica, documents
dramatic swings in hydroclimate over the past few millennia. However, the dynamics …

Dust events originating from the Saharan desert have far‐reaching environmental impacts,
but the causal mechanism of magnitude and occurrence of Saharan dust events (SDEs) …

Epikarst estuary response to hydroclimate change remains poorly understood, despite the
well-studied link between climate and karst groundwater aquifers. The influence of sea-level …