Global climate models, indispensable for projecting the human-driven climate change, have
been improving for decades and are nowadays capable of reproducing multiple processes …

Multiple studies have considered whether increased anthropogenic CO2 will affect the wind
speeds and turbulence associated with the winter North Atlantic polar‐front jet stream in the …

In wintertime over the subpolar North Atlantic Ocean (SPNA), the strongest surface sensible
and latent heat fluxes typically occur just downstream of the sea‐ice edge. The recent retreat …

Atmospheric rivers (ARs) are filamentary conduits of intense moisture transport crucial for
water delivery to mid‐latitude coastal regions. How ARs have responded to extratropical …

The global acceleration of sea-level rise (SLR) during the 20th century is now established.
On the local scale, this is harder to establish as several drivers of SLR play a role, which can …

Abstract Information from a variety of sources has suggested that increased storminess was
experienced across the British Isles in the late eighteenth/early nineteenth century …

The quasi-periodic signals in the earth system could be the predictability source for sub-
seasonal to seasonal (S2S) climate prediction because of the connections among the lead …

The effect of Arctic sea ice loss on the boreal winter regional trends of wind speed and
latitudinal position of the Northern Hemisphere subtropical jet stream (STJ) in 1980–2012 is …

The underlying dynamics controlling jet streams are complex, but it is expected that they will
have an observable response to changes in the larger climatic system. A growing …

Abstract The North Atlantic jet stream (NAJ) has a profound impact on the climate of the
North Atlantic–European sector, especially in winter. Observations show that the winter NAJ …