Will there by some sudden impact upon a BOE? Science says no.
Here is a reconstructed history of ice in the Arctic:
https://www.google.com/url?sa=t&rct=j&q=&esrc=s&source=web&cd=&cad=rja&uact=8&ved=2ahUKEwin6rWO5bHvAhWx3OAKHXiMCNEQFjAKegQIChAF&url=https%3A%2F%2Fwww.geo.umass.edu%2Ffaculty%2Fjbg%2FPubs%2FPolyak%2520etal%2520seaice%2520QSR10%2520inpress.pdf&usg=AOvVaw1zyrQLvhkjRUiwHYh2lWMWSome quotes indicating that
during the Eemian and Holocene Optimum, there was very little ice during summer (and as we know this did NOT lead to some unstoppable kind of climate catastrophe):
"interglacial and major
interstadial intervals are characterized by higher marine productivity
suggestive of reduced ice cover. The most prominent evidence
is that
planktonic foraminifers typical of subpolar, seasonally open
water lived in the central Arctic Ocean during the last interglacial(MIS 5e)...given that
one of these areas, north of Greenland, is presently characterized by
especially thick and widespread ice,
most of the Arctic Ocean may
have been free of summer ice cover during these intervals"
"intertidal snails found near Nome, just
south of the
Bering Strait, suggest that the coast there may have
been annually ice-free"
"Deposits near Barrow include at least one
mollusk and several ostracode species known now only from the
North Atlantic."
Holocene optimum:
"Probably the most spectacular evidence of low-ice Arctic
conditions in the early Holocene comes from Northeast Greenland
(Fig. 8; Funder and Kjær, 2007; Funder et al., 2009). At this northernmost
coast in the world, isostatically raised ‘staircases’ of welldeveloped
wave-generated beach ridges investigated along a total
coastline stretch of several hundred kilometers document seasonally
openwater
as far north as 83oN....
Presently the entire Northeast Greenland coastline is permanently
surrounded by pack ice with numerous pressure ridges and rare
locked-in icebergs, with coastal melt occurring maximum to 76oN"
"Bowhead bones
are most commonly found in all three CAA regions in early Holocene
deposits,
11–9 cal. ka. At that time Pacific and Atlantic bowheads
were clearly able to intermingle freely along the length of the
Northwest Passage, indicating at least periodically ice-free
summers."
"A more continuous reconstruction of ice conditions in central
CAA is now available based on IP25, a biomarker of ice-related
diatom spring blooms (Vare et al., 2009).
A downcore IP25 record
from the central archipelago demonstrates little ice during the early
Holocene, an accelerating increase in ice occurrence between 6 and
3 ka, and high but variable occurrence since then"