Reply to discussion on 'Deglaciation and neotectonics in SE Raasay, Scottish Inner Hebrides’ by Smith et al. 2021 (SJG, 57, 106-116)

2021 ◽  
pp. sjg2021-014
Author(s):  
David E. Smith ◽  
Callum R Firth ◽  
Timothy M. Mighall ◽  
Phillip Teasdale
Keyword(s):  

We greatly appreciate Dr Morton's interest in our paper and his appreciative comments. The features at Beinn na Leac are, in our opinion, of particular interest to geologists interested in the pattern of deglaciation and neotectonics in this part of western Scotland. The location is unique in Scotland in the magnitude of Younger Dryas/Holocene fault dislocation. We respond to Dr Morton's comments as follows:

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Brice R. Rea ◽  
Ramón Pellitero ◽  
Matteo Spagnolo ◽  
Philip Hughes ◽  
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The Younger Dryas (YD) was a period of rapid climate cooling that occurred at the end of the last glaciation. Here, we present the first palaeoglacier-derived reconstruction of YD precipitation across Europe, determined from 122 reconstructed glaciers and proxy atmospheric temperatures. Positive precipitation anomalies (YD versus modern) are found along much of the western seaboard of Europe and across the Mediterranean. Negative precipitation anomalies occur over the Fennoscandian ice sheet, the North European Plain, and as far south as the Alps. This is consistent with a more southerly and zonal storm track, which is linked to a concomitant southern location of the Polar Frontal Jet Stream, generating cold air outbreaks and enhanced cyclogenesis, especially over the eastern Mediterranean. This atmospheric configuration resembles the modern Scandinavian (SCAND) circulation over Europe (a blocking high pressure over Scandinavia pushing storm tracks south and east), and by analogy, a seasonally varying palaeoprecipitation pattern is interpreted.


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Vol 3 (1) ◽  
pp. 1-19 ◽  
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Vol 432 ◽  
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Yancheng Zhang ◽  
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Stefan Mulitza ◽  
Matthias Zabel ◽  
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...  

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