Each occasion made
difficult by ice / snow / wind.
Not exact matches
By using theoretical simulations, the researchers were able to model states of superionic
ice that would be
difficult to study experimentally.
One of the Science co-authors, Peter Huybers, a climate scientist at Harvard University, says he was pleased
by the confirmation — especially because it comes from a fast - spreading center, where the
ice age signal is more
difficult to observe.
It is
difficult to obtain fossil data from the 10 % of Earth's terrestrial surface that is covered
by thick glaciers and
ice sheets, and hence, knowledge of the paleoenvironments of these regions has remained limited.
Climate change models predict that the Arctic sea
ice will continue to shrink in a warming world (as much as 40 % of the
ice is expected to be gone
by midcentury), and the resulting changes — including later formation of
ice in the autumn, rain falling on the snow, and decreasing snow depths — will make it increasingly
difficult for the seals to construct their snow caves, NOAA says.
Rather the cores require a more complicated analysis that is becoming more
difficult by the day as the
ice melts.
Solar forcing has been suggested for the Mayans and for the Little
Ice Age, but hard evidence is
difficult to come
by.
It remains
difficult to assess how soon a collapse of Pine Island Glacier could occur, but a new paper
by Bamber and Aspinall (2013) suggest that there is a growing view that the West Antarctic
Ice Sheet could become unstable over the next 100 years16.
Based on the candid and sometimes startling conversations that YOU were never meant to hear, THE TONYA TAPES, written
by award - winning author Lynda D. Prouse, chronicles the life of the world's most infamous female athlete — TONYA HARDING — revealing for the first time the whole truth of her
difficult and amazing life on and off the
ice.
Today's feature flick has a GT - R hitting 183 mph, but Nissan made things more
difficult by doing the entire test on
ice.
It is
difficult for many people (including some geologists) to visualize how sea level could drop that much just
by expanding the
ice caps.
It is
difficult to see how a person in the general public should not be concerned
by the downward trend of Arctic sea
ice volume.
This can become
difficult since the
ice chronologies can only be checked
by finding and definitively identifying tephra (volcanic glass shards) that can be attributed to these key eruptions; sulphate peaks in the
ice are not volcano specific.
They plan to drill short
ice core samples and analyze the past role of black carbon, including layers from 2012 (though Doherty points out that it may be
difficult to tell how much black carbon was deposited then, rather than deposited in earlier years and concentrated
by the melting).
What I find
difficult with the «other» paper that it is again an a-posteriors explanation (like cold European winters caused
by less Arctic sea
ice in the preceding fall) and just one.
It would be rather
difficult to see increasing sea
ice from the AMO and achieve an
ice free Arctic ocean
by 2050.
Modern day data on what is happening beneath the
ice sheets is
difficult to come
by.
Mark Serreze, the director of the NSIDC, said that making a clear separation between manmade and natural factors is «very
difficult,» since as the sea
ice thins, it become more vulnerable to melting spurred
by weather patterns.
Thin
ice makes it more
difficult to rely on conventional wisdom, although this year has proven that a lack of melting momentum during May and June followed
by weather conditions during July and August that do not favour melt / export / compaction can still prevent a record, even if volume was at a record low for much of the year.
However, detecting acceleration is
difficult because of (i) interannual variability in GMSL largely driven
by changes in terrestrial water storage (TWS)(7 ⇓ — 9), (ii) decadal variability in TWS (10), thermosteric sea level, and
ice sheet mass loss (11) that might masquerade as a long - term acceleration over a 25 - y record, (iii) episodic variability driven
by large volcanic eruptions (12), and (iv) errors in the altimeter data, in particular, potential drifts in the instruments over time (13).
Reports
by Joe Leavitt, a Barrow
ice expert, indicate that the prevailing winds have been pushing
ice offshore, making access to sea
ice for hunting
difficult along the Chukchi coast.