Hundreds of coral paleoclimate records have been developed over the past several
decades, significantly extending the instrumental record and improving our understanding of …

Kelp forests are declining in many regions globally with climatic perturbations causing shifts
to alternate communities and significant ecological and economic loss. Range edge …

Trace element abundances in corals can potentially provide high-resolution seasonally
resolved constraints on past sea-surface temperatures, much needed to improve our …

Extreme events such as Marine Heat Waves (MHWs) and Low Chlorophyll-a (LChl-a) in the
ocean have devastating impacts on the marine environment, particularly when they occur …

Abstract The Akkadian Empire was the first united empire in Mesopotamia and was
established at 4.6 kyr BP (where present is AD 1950). The empire abruptly collapsed in …

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 …

Sea surface temperature (SST) and isothermal layer depth (ILD) are important oceanic
parameters and could play a significant role in understanding the upper thermal structure as …

Abstract Upwelling in the Arabian Sea driven by the Indian summer monsoon pumps deep,
cold, and eutrophic seawater to the sea surface every summer. The Indian summer …

Coral skeletons are the most commonly used high‐resolution temperature proxy in the
tropical oceans, providing paleoclimate reconstructions dating back centuries to millennia …

The skeletons of massive corals inhabiting tropical and subtropical oceans grow over
centuries. The chemical and isotopic compositions of their skeletons reflect changes in the …