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| Started by | Sam Wormley <swormley1@gmail.com> |
|---|---|
| First post | 2016-02-12 16:18 -0600 |
| Last post | 2016-02-12 20:20 -0600 |
| Articles | 7 — 3 participants |
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Study: Ice-Shelf Loss Leads To Faster Sea Level Rise Sam Wormley <swormley1@gmail.com> - 2016-02-12 16:18 -0600
Re: Study: Ice-Shelf Loss Leads To Faster Sea Level Rise jimp@specsol.spam.sux.com - 2016-02-12 22:49 +0000
Re: Study: Ice-Shelf Loss Leads To Faster Sea Level Rise Sam Wormley <swormley1@gmail.com> - 2016-02-12 20:13 -0600
Re: Study: Ice-Shelf Loss Leads To Faster Sea Level Rise jimp@specsol.spam.sux.com - 2016-02-13 03:38 +0000
Re: Study: Ice-Shelf Loss Leads To Faster Sea Level Rise Sam Wormley <swormley1@gmail.com> - 2016-02-13 08:24 -0600
Re: Study: Ice-Shelf Loss Leads To Faster Sea Level Rise Sam Wormley <swormley1@gmail.com> - 2016-02-13 13:10 -0600
Re: Study: Ice-Shelf Loss Leads To Faster Sea Level Rise Sergio <invalid@invalid.com> - 2016-02-12 20:20 -0600
| From | Sam Wormley <swormley1@gmail.com> |
|---|---|
| Date | 2016-02-12 16:18 -0600 |
| Subject | Study: Ice-Shelf Loss Leads To Faster Sea Level Rise |
| Message-ID | <KcydnUVUoN22xyPLnZ2dnUU7-X2dnZ2d@giganews.com> |
Study: Ice-Shelf Loss Leads To Faster Sea Level Rise > http://www.reportingclimatescience.com/news-stories/article/study-ice-shelf-loss-leads-to-faster-sea-level-rise.html > Abstract > > The floating ice shelves along the seaboard of the Antarctic ice > sheet restrain the outflow of upstream grounded ice. Removal of these > ice shelves, as shown by past ice-shelf recession and break-up, > accelerates the outflow, which adds to sea-level rise. A key question > in predicting future outflow is to quantify the extent of calving > that might precondition other dynamic consequences and lead to loss > of ice-shelf restraint. Here we delineate frontal areas that we label > as ‘passive shelf ice’ and that can be removed without major dynamic > implications, with contrasting results across the continent. The ice > shelves in the Amundsen and Bellingshausen seas have limited or > almost no ‘passive’ portion, which implies that further retreat of > current ice-shelf fronts will yield important dynamic consequences. > This region is particularly vulnerable as ice shelves have been > thinning at high rates for two decades and as upstream grounded ice > rests on a backward sloping bed, a precondition to marine ice-sheet > instability. In contrast to these ice shelves, Larsen C Ice Shelf, in > the Weddell Sea, exhibits a large ‘passive’ frontal area, suggesting > that the imminent calving of a vast tabular iceberg will be unlikely > to instantly produce much dynamic change. > > Citation > > The safety band of Antarctic ice shelves by Johannes Jakob Fürst, > Gaël Durand, Fabien Gillet-Chaulet, Laure Tavard, Melanie Rankl, > Matthias Braun and Olivier Gagliardini, published in Nature Climate > Change, DOI: 10.1038/NCLIMATE2912 > -- sci.physics is an unmoderated newsgroup dedicated to the discussion of physics, news from the physics community, and physics-related social issues.
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| From | jimp@specsol.spam.sux.com |
|---|---|
| Date | 2016-02-12 22:49 +0000 |
| Message-ID | <2442pc-7qq.ln1@mail.specsol.com> |
| In reply to | #552623 |
Sam Wormley <swormley1@gmail.com> wrote: > Study: Ice-Shelf Loss Leads To Faster Sea Level Rise Too bad you didn't cut and paste this to a group where it would be appropriate, spammer. -- Jim Pennino
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| From | Sam Wormley <swormley1@gmail.com> |
|---|---|
| Date | 2016-02-12 20:13 -0600 |
| Message-ID | <KcydnUJUoN2uDCPLnZ2dnUU7-X2dnZ2d@giganews.com> |
| In reply to | #552632 |
On 2/12/16 4:49 PM, jimp@specsol.spam.sux.com wrote: > Too bad you didn't cut and paste this to a group where it would be > appropriate, spammer. Now, now, jimp, your *obsessive-compulsive* behavior is outta control, your *language inappropriate* and your absolute contempt and total disgust are addressed in these Anger Management classes. You, jimp, need these services: > http://yellowpages.com/rancho-cucamonga-ca/anger-management-classes Study: Ice-Shelf Loss Leads To Faster Sea Level Rise > http://www.reportingclimatescience.com/news-stories/article/study-ice-shelf-loss-leads-to-faster-sea-level-rise.html > Abstract > > The floating ice shelves along the seaboard of the Antarctic ice > sheet restrain the outflow of upstream grounded ice. Removal of these > ice shelves, as shown by past ice-shelf recession and break-up, > accelerates the outflow, which adds to sea-level rise. A key question > in predicting future outflow is to quantify the extent of calving > that might precondition other dynamic consequences and lead to loss > of ice-shelf restraint. Here we delineate frontal areas that we label > as ‘passive shelf ice’ and that can be removed without major dynamic > implications, with contrasting results across the continent. The ice > shelves in the Amundsen and Bellingshausen seas have limited or > almost no ‘passive’ portion, which implies that further retreat of > current ice-shelf fronts will yield important dynamic consequences. > This region is particularly vulnerable as ice shelves have been > thinning at high rates for two decades and as upstream grounded ice > rests on a backward sloping bed, a precondition to marine ice-sheet > instability. In contrast to these ice shelves, Larsen C Ice Shelf, in > the Weddell Sea, exhibits a large ‘passive’ frontal area, suggesting > that the imminent calving of a vast tabular iceberg will be unlikely > to instantly produce much dynamic change. > > Citation > > The safety band of Antarctic ice shelves by Johannes Jakob Fürst, > Gaël Durand, Fabien Gillet-Chaulet, Laure Tavard, Melanie Rankl, > Matthias Braun and Olivier Gagliardini, published in Nature Climate > Change, DOI: 10.1038/NCLIMATE2912 > -- sci.physics is an unmoderated newsgroup dedicated to the discussion of physics, news from the physics community, and physics-related social issues.
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| From | jimp@specsol.spam.sux.com |
|---|---|
| Date | 2016-02-13 03:38 +0000 |
| Message-ID | <o1l2pc-phs.ln1@mail.specsol.com> |
| In reply to | #552683 |
Sam Wormley <swormley1@gmail.com> wrote: > On 2/12/16 4:49 PM, jimp@specsol.spam.sux.com wrote: >> Too bad you didn't cut and paste this to a group where it would be >> appropriate, spammer. > > > Now, now, jimp, your *obsessive-compulsive* behavior is outta control, Too bad you didn't cut and paste this to a group where it would be appropriate, spammer. Fuck off and die, shit head. -- Jim Pennino
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| From | Sam Wormley <swormley1@gmail.com> |
|---|---|
| Date | 2016-02-13 08:24 -0600 |
| Message-ID | <E6ednRQeU6MsoSLLnZ2dnUU7-Y3OydjZ@giganews.com> |
| In reply to | #552734 |
On 2/12/16 9:38 PM, jimp@specsol.spam.sux.com wrote: > Fuck off and die, shit head Now, now, jimp, your *obsessive-compulsive* behavior is outta control, your *language inappropriate* and your absolute contempt and total disgust are addressed in these Anger Management classes. You, jimp, need these services: > http://yellowpages.com/rancho-cucamonga-ca/anger-management-classes Study: Ice-Shelf Loss Leads To Faster Sea Level Rise > http://www.reportingclimatescience.com/news-stories/article/study-ice-shelf-loss-leads-to-faster-sea-level-rise.html > Abstract > > The floating ice shelves along the seaboard of the Antarctic ice > sheet restrain the outflow of upstream grounded ice. Removal of these > ice shelves, as shown by past ice-shelf recession and break-up, > accelerates the outflow, which adds to sea-level rise. A key question > in predicting future outflow is to quantify the extent of calving > that might precondition other dynamic consequences and lead to loss > of ice-shelf restraint. Here we delineate frontal areas that we label > as ‘passive shelf ice’ and that can be removed without major dynamic > implications, with contrasting results across the continent. The ice > shelves in the Amundsen and Bellingshausen seas have limited or > almost no ‘passive’ portion, which implies that further retreat of > current ice-shelf fronts will yield important dynamic consequences. > This region is particularly vulnerable as ice shelves have been > thinning at high rates for two decades and as upstream grounded ice > rests on a backward sloping bed, a precondition to marine ice-sheet > instability. In contrast to these ice shelves, Larsen C Ice Shelf, in > the Weddell Sea, exhibits a large ‘passive’ frontal area, suggesting > that the imminent calving of a vast tabular iceberg will be unlikely > to instantly produce much dynamic change. > > Citation > > The safety band of Antarctic ice shelves by Johannes Jakob Fürst, > Gaël Durand, Fabien Gillet-Chaulet, Laure Tavard, Melanie Rankl, > Matthias Braun and Olivier Gagliardini, published in Nature Climate > Change, DOI: 10.1038/NCLIMATE2912 > -- sci.physics is an unmoderated newsgroup dedicated to the discussion of physics, news from the physics community, and physics-related social issues.
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| From | Sam Wormley <swormley1@gmail.com> |
|---|---|
| Date | 2016-02-13 13:10 -0600 |
| Message-ID | <OaKdnf4lR_Q14iLLnZ2dnUU7-e-dnZ2d@giganews.com> |
| In reply to | #552782 |
On 2/13/16 12:55 PM, jimp@specsol.spam.sux.com wrote: > Fuck off and die, shit head Now, now, jimp, your *obsessive-compulsive* behavior is outta control, your *language inappropriate* and your absolute contempt and total disgust are addressed in these Anger Management classes. You, jimp, need these services: > http://yellowpages.com/rancho-cucamonga-ca/anger-management-classes Study: Ice-Shelf Loss Leads To Faster Sea Level Rise > http://www.reportingclimatescience.com/news-stories/article/study-ice-shelf-loss-leads-to-faster-sea-level-rise.html > Abstract > > The floating ice shelves along the seaboard of the Antarctic ice > sheet restrain the outflow of upstream grounded ice. Removal of these > ice shelves, as shown by past ice-shelf recession and break-up, > accelerates the outflow, which adds to sea-level rise. A key question > in predicting future outflow is to quantify the extent of calving > that might precondition other dynamic consequences and lead to loss > of ice-shelf restraint. Here we delineate frontal areas that we label > as ‘passive shelf ice’ and that can be removed without major dynamic > implications, with contrasting results across the continent. The ice > shelves in the Amundsen and Bellingshausen seas have limited or > almost no ‘passive’ portion, which implies that further retreat of > current ice-shelf fronts will yield important dynamic consequences. > This region is particularly vulnerable as ice shelves have been > thinning at high rates for two decades and as upstream grounded ice > rests on a backward sloping bed, a precondition to marine ice-sheet > instability. In contrast to these ice shelves, Larsen C Ice Shelf, in > the Weddell Sea, exhibits a large ‘passive’ frontal area, suggesting > that the imminent calving of a vast tabular iceberg will be unlikely > to instantly produce much dynamic change. > > Citation > > The safety band of Antarctic ice shelves by Johannes Jakob Fürst, > Gaël Durand, Fabien Gillet-Chaulet, Laure Tavard, Melanie Rankl, > Matthias Braun and Olivier Gagliardini, published in Nature Climate > Change, DOI: 10.1038/NCLIMATE2912 > -- sci.physics is an unmoderated newsgroup dedicated to the discussion of physics, news from the physics community, and physics-related social issues.
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| From | Sergio <invalid@invalid.com> |
|---|---|
| Date | 2016-02-12 20:20 -0600 |
| Message-ID | <n9m3u2$115e$1@gioia.aioe.org> |
| In reply to | #552623 |
On 2/12/2016 4:18 PM, Sam Wormley wrote: > Study: Ice-Shelf Loss Leads To Faster Sea Level Rise another bullshit article; "Removal of these ice shelves, as shown by past ice-shelf recession and break-up, accelerates the outflow, which adds to sea-level rise." their assumption is more water down the stream, makes the sea level rise, bad assumption.
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