Peter M Abbott

Ice melt, sea level rise and superstorms: evidence from paleoclimate data, climate modeling, and modern observations that 2 °C global warming could be dangerous

The Arctic has warmed nearly four times faster than the globe since 1979

Defining the Anthropocene

Modeling the Age of the Cape Riva (Y-2) Tephra

Quaternary Sea-Level Changes: A Global Perspective

Flexible paleoclimate age-depth models using an autoregressive gamma process

Climate drivers for peatland palaeoclimate records

COOPERATION CONTRACT IN TOURISM SUPPLY CHAINS: THE OPTIMAL PRICING STRATEGY OF HOTELS FOR COOPERATIVE THIRD PARTY STRATEGIC WEBSITES

Precise ¹⁴C ages of the Vedde and Saksunarvatn ashes and the Younger Dryas boundaries from western Norway and their comparison with the Greenland Ice Core (GICC05) chronology

Trajectories of the Earth System in the Anthropocene

Flexible paleoclimate age-depth models using an autoregressive gamma process

The role of cryptotephra in refining the chronology of Late Pleistocene human evolution and cultural change in North Africa

Coordination of channel members’ efforts and utilities in contract farming operations

Methods and code for ‘classical’ age-modelling of radiocarbon sequences

Pleistocene North African genomes link Near Eastern and sub-Saharan African human populations

The State of the World's Mangrove Forests: Past, Present, and Future

Past perspectives on the present era of abrupt Arctic climate change

Assessing the differences between the IntCal and Greenland ice-core time scales for the last 14,000 years via the common cosmogenic radionuclide variations

Volcanic markers for dating the onset of the Anthropocene

Deglaciation of Fennoscandia

Recent and Planned Developments of the Program OxCal

Were last glacial climate events simultaneous between Greenland and France? A quantitative comparison using non‐tuned chronologies

Volcanism and the Greenland ice-cores: the tephra record

Tracing volcanic events in the NGRIP ice-core and synchronising North Atlantic marine records during the last glacial period

Consistently dated records from the Greenland GRIP, GISP2 and NGRIP ice cores for the past 104 ka reveal regional millennial-scale δ18O gradients with possible Heinrich event imprint

Front Office: Procedures, Social Skills, Yield And Management

Integrating the INTIMATE records using tephrochronology: rising to the challenge

Comment: Were last glacial climate events simultaneous between Greenland and France? A quantitative comparison using non‐tuned chronologies. M. Blaauw, B. Wohlfarth, J. A. Christen, L. Ampel, D. Veres, K. Hughen, F. Preusser and A. Svensson (2009)