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Redefining lithic microdebitage with experimental archaeology
Lithic microdebitage is “invisible” to the naked eye. Since ancient knappers struggled to remove it from activity areas, its presence can reveal...
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Working Approach: Field Investigation
The present chapter highlighted the preliminary approach for palaeoclimate studies using lake sediments and discussed the importance of proxy...
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Neutron activation analysis in Mediterranean Archaeology: current applications and future perspectives
This paper, jointly written by participants of a workshop held in 2021, argues for an increased recognition and application of neutron activation...
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Spatial-temporal dynamics of alpine grassland coverage and its response to climate warming in Mt. Qomolangma Nature Preserve during 2000–2019
The Qinghai–Tibet Plateau (QTP) has the largest and highest alpine grassland ecosystem in the world, which is considered to be the most sensitive and...
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Possible widths of Indian summer monsoon trajectories in Tibetan Plateau revealed by the direction of maximum summer precipitation decreases in recent decades
The Tibetan Plateau (TP) affects its surrounding regions through thermal and dynamic processes. Hydrological cycles in TP are experiencing dramatic...
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The Dynamic Evolution of Permeability in Compacting Carbonates: Phase Transition and Critical Points
Mechanical damage and resultant permeability evolution during compaction of highly porous reservoir rocks have strong implications on the extraction...
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Millennial and centennial CO2 release from the Southern Ocean during the last deglaciation
For its greenhouse effects, atmospheric CO 2 can critically influence the global climate on millennial and centennial timescales. Pleistocene...
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An Attention-Based Temporal and Spatial Convolution Recursive Neural Network for Surrogate Modeling of the Production Curve Prediction
Reservoir numerical simulation is a time-consuming and expensive procedure, especially for production optimization and history matching, which...
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A Review of El Niño Southern Oscillation Linkage to Strong Volcanic Eruptions and Post-Volcanic Winter Warming
Understanding the influence of volcanism on ENSO and associated climatic impacts is of great scientific and social importance. Although many studies...
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Map** and monitoring peatland conditions from global to field scale
Peatlands cover only 3–4% of the Earth’s surface, but they store nearly 30% of global soil carbon stock. This significant carbon store is under...
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Monitoring cyanobacterial blooms: a strategy combining predictive modeling and remote sensing approaches
Development of effective monitoring programs and early alert systems of cyanobacterial harmful blooms (CyanoHABs) is a challenge due to their rapid...
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Identifying biological affinities of Holocene northern Iberian populations through the inner structures of the upper first molars
Neolithisation was a relatively fast process that affected both the interior and coastal zones of the Iberian Peninsula, but it was also a...
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Higher quantiles of sea levels rise faster in Baltic Sea Climate projections
Absolute sea levels in the Baltic Sea will rise under the influence of climate warming, similar to those in the world ocean. For extreme sea levels,...
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Distinctive changes of Asian–African summer monsoon in interglacial epochs and global warming scenario
Precipitation was claimed to increase over Asian–African summer monsoon (AAM) regions during past interglacial epochs and also under future global...
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Assisted Upscaling of Miscible CO2-Enhanced Oil Recovery Floods Using an Artificial Neural Network-Based Optimisation Algorithm
Due to the high computing cost of the fine-scale compositional simulations needed to effectively model miscible CO 2 flooding, upscaling techniques...
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Impacts of tropical cyclones and anthropogenic activities on marine vanadium: A unique perspective from high resolution Porites coral record
As a typical contaminant in fossil fuels, vanadium has undergone dramatically increase due to the impacts from human activities. The excessive...
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Mid-Pliocene glaciation preceded by a 0.5-million-year North African humid period
Past North African humid periods caused expanded vegetation over the Sahara, due to northward tropical African rainbelt displacement, opening...
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Increased water vapor supply in winter and spring leading to the arid Central Asian wetting in last 6000 years
Paleoclimate reconstructions show that the arid Central Asia (ACA) is characterized by a wetting trend from the mid-Holocene (MH) to the...
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Polar jet stream fluctuations in an energy balance model
We investigate the effect of increased longwave radiative forcing (a proxy for increased greenhouse gas concentration) on the zonally averaged...
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Mechanisms for African easterly wave changes in simulations of the mid-Holocene
The mid-Holocene was a warm period with significantly amplified precipitation in North Africa, and a northward shifted Western African Monsoon during...
