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

The temperate region of Western Europe underwent dramatic climatic and environmental
change during the last deglaciation. Much of what is known about the terrestrial ecosystem …

Stable water isotopes in polar ice cores are widely used to reconstruct past temperature
variations over several orbital climatic cycles. One way to calibrate the isotope–temperature …

Improving the understanding of changes in the mean and variability of climate variables as
well as their interrelation is crucial for reliable climate change projections. Comparisons …

The incorporation of water isotopologues into the hydrology of general circulation models
(GCMs) facilitates the comparison between modeled and measured proxy data 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 …

Reconstructing of past hydroclimates at regional scales during the Common Era (CE) is
necessary to place the current warming in the context of natural climate variability. Here we …

Reconstruction of past changes in monsoon climate from speleothem oxygen isotope (δ 18
O) records is complex because δ 18 O signals can be influenced by multiple factors …

The climate impact contribution of lakes to sustain the Green Sahara in the mid-Holocene
(MH, 6000 years ago) is still under debate. To assess the lake-induced climate response …

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