Ocean Feedback in Response to 6 kyr BP Insolation

Millennial scale changes in sea surface temperature and ocean circulation in the northeast Pacific, 10–60 kyr BP

[1] A new centennial-scale Mg/Ca temperature record from the California margin (ODP Site 1017E) reveals large millennial-scale oscillations between 10 to 60 kyr. This record indicates that sea surface temperature on the California Margin warmed rapidly on the deglacial by 7.4 0.8 C, and was preceded by a pre-Bølling temperature oscillation of 2.6 1.2 C. Millennial-scale events of the last glaci...

Glacial lake drainage in Patagonia (13-8 kyr) and response of the adjacent Pacific Ocean

Large freshwater lakes formed in North America and Europe during deglaciation following the Last Glacial Maximum. Rapid drainage of these lakes into the Oceans resulted in abrupt perturbations in climate, including the Younger Dryas and 8.2 kyr cooling events. In the mid-latitudes of the Southern Hemisphere major glacial lakes also formed and drained during deglaciation but little is known abou...

: examining l2 teachers’ corrective feedback types in relation to learners’ uptake, proficiency levels, and context types

abstract this study investigates the teachers’ correction of students’ spoken errors of linguistic forms in efl classes, aiming at (a) examining the relationship between the learners’ proficiency level and the provision of corrective feedback types, (b) exploring the extent to which teachers’ use of different corrective feedback types is related to the immediate types of context in which err...

Typhoon-Ocean Interaction: The Ocean Response to Typhoons, and Its Feedback to Typhoon Intensity – Synergy of Observations and Model Simulations

Moisture - advection feedback supports strong early - to - mid Holocene monsoon 1 climate on the eastern Tibetan Plateau as inferred from a pollen - based 2 reconstruction 3 4

32 (Paleo-)climatologists are challenged to identify mechanisms that cause the 33 observed abrupt Holocene monsoon events despite the fact that monsoonal 34 circulation is assumed to be driven by gradual insolation changes. Here we provide 35 proxy and model evidence to show that moisture-advection feedback can lead to a 36 non-linear relationship between sea-surface and continental temperature...