Thank you for using the timer - this advanced tool can estimate your performance and suggest more practice questions. We have subscribed you to Daily Prep Questions via email.
Customized for You
we will pick new questions that match your level based on your Timer History
Track Your Progress
every week, we’ll send you an estimated GMAT score based on your performance
Practice Pays
we will pick new questions that match your level based on your Timer History
Not interested in getting valuable practice questions and articles delivered to your email? No problem, unsubscribe here.
Thank you for using the timer!
We noticed you are actually not timing your practice. Click the START button first next time you use the timer.
There are many benefits to timing your practice, including:
Do RC/MSR passages scare you? e-GMAT is conducting a masterclass to help you learn – Learn effective reading strategies Tackle difficult RC & MSR with confidence Excel in timed test environment
Prefer video-based learning? The Target Test Prep OnDemand course is a one-of-a-kind video masterclass featuring 400 hours of lecture-style teaching by Scott Woodbury-Stewart, founder of Target Test Prep and one of the most accomplished GMAT instructors.
Scientists have long assumed that Antarctic ice sheets are essentially stable. In theory, snowfall replenishes ice sheets, replacing the mass lost when ice from the sheets flows outward in solid streams and sheds into the oceam as icebergs. However, satellite measurements show that the West Antarctic ice sheet has been losing mass and that its ice streams are accelerating.
To explain these changes, geophysicist Robin Bell and her colleagues have been studying the role played by liquid water under the ice sheet. They have found that although the base of the ice sheet is insulated from changing atmospheric temperatures, it can melt because of friction as it moves over underlying rock. The meltwater lubricates and accelerates the ice streams. Furthermore, some lakes below the ice sheets are draining, adding more lubrication that further destabilizes the streams.
Ordinarily, ice streams cause ice shelves to accumulate at the streams' oceam outlets. These shelves block and slow the streams. But since ice shelves are sensitive to ocean temperatures, global warming can melt them. In 2002, ice streams flowing into Larsen B ice shelf in West Antarctica accelerated dramatically after much of the shelf collapsed into the ocean. This suggests that global warming could allow far more land-based ice to flow into the ocean, raising sea levels rapidly.
PS I'm not able to add the qns here. Requesting expert help here on these qn explanations via these screenshots.
Archived Topic
Hi there,
This topic has been closed and archived due to inactivity or violation of community quality standards. No more replies are possible here.
Still interested in this question? Check out the "Best Topics" block below for a better discussion on this exact question, as well as several more related questions.
Scientists have long assumed that Antarctic ice sheets are essentially stable. In theory, snowfall replenishes ice sheets, replacing the mass lost when ice from the sheets flows outward in solid streams and sheds into the oceam as icebergs. However, satellite measurements show that the West Antarctic ice sheet has been losing mass and that its ice streams are accelerating.
To explain these changes, geophysicist Robin Bell and her colleagues have been studying the role played by liquid water under the ice sheet. They have found that although the base of the ice sheet is insulated from changing atmospheric temperatures, it can melt because of friction as it moves over underlying rock. The meltwater lubricates and accelerates the ice streams. Furthermore, some lakes below the ice sheets are draining, adding more lubrication that further destabilizes the streams.
Ordinarily, ice streams cause ice shelves to accumulate at the streams' oceam outlets. These shelves block and slow the streams. But since ice shelves are sensitive to ocean temperatures, global warming can melt them. In 2002, ice streams flowing into Larsen B ice shelf in West Antarctica accelerated dramatically after much of the shelf collapsed into the ocean. This suggests that global warming could allow far more land-based ice to flow into the ocean, raising sea levels rapidly.
PS I'm not able to add the qns here. Requesting expert help here on these qn explanations via these screenshots.
Show more
Posted here: https://gmatclub.com/forum/scientists-have-long-assumed-that-antarctic-ice-sheets-are-essentially-427456.html Please check there the correct wy of posting RC. Hope it helps.
Archived Topic
Hi there,
This topic has been closed and archived due to inactivity or violation of community quality standards. No more replies are possible here.
Still interested in this question? Check out the "Best Topics" block above for a better discussion on this exact question, as well as several more related questions.