cryo-sea Earth Science

2 个科学问题 · 地球科学 Earth Science

本页目录

漂浮的冰架崩解入海并不会直接抬高海平面,科学家为什么仍把它视为海平面上升的重大警报?

Calving of floating ice shelves does not itself raise sea level, so why do scientists treat their collapse as a major sea-level alarm?

冰架漂浮时排开的海水体积与其自身质量相当,崩解或融化并不直接改变海平面;但冰架如同闸门,约束着后方陆地冰流的速度。拉森B冰架于2002年解体后,原本受其阻挡的冰川流速成倍加快,更多的陆地冰被送入海洋,这部分质量转移才是海平面上升的直接来源。
While floating, an ice shelf displaces seawater equal to its own mass, so its breakup adds nothing directly to sea level; the concern is that shelves buttress the grounded ice behind them. After Larsen B disintegrated in 2002, the tributary glaciers it restrained accelerated severalfold, flushing more land ice into the ocean — and that transfer of mass is what actually lifts sea level.
难度 进阶 · 适合 初中(12-15) CC BY 4.0 · 已核验 · Verified 2026-11-02
来源 · Source

Rignot 等 2004 年发表于 Geophysical Research Letters 的论文:拉森B冰架崩塌后南极半岛冰流加速

Rignot, E. et al., Geophysical Research Letters, 2004: Accelerated ice discharge from the Antarctic Peninsula following the collapse of Larsen B ice shelf

#冰架崩解 #海平面贡献

末次冰期的巨厚冰盖消融已逾万年,波罗的海与哈得孙湾沿岸为何至今仍在可测地抬升?这又如何扭曲当地验潮站的相对海平面趋势?

The vast ice sheets of the last glacial age melted away more than ten thousand years ago, so why are the coasts of the Baltic and Hudson Bay still measurably rising, and how does that warp relative sea-level trends read from local tide gauges?

数千米的冰盖曾把岩石圈压弯,并将地幔物质挤向四周;冰雪消融后地幔开始黏弹性回弹,恢复过程延续至今。陆地抬升快于海面之处,验潮站记录到的海平面下降其实是岸线上升的假象。而在原冰盖外围的前缘隆起带,回流的地幔物质导致地面下沉,当地相对海平面反而升得比全球平均更快。
Ice sheets kilometers thick bowed the lithosphere downward and squeezed mantle material sideways; once the ice vanished, the mantle began a viscous rebound that continues today. Wherever land climbs faster than the sea surface, tide gauges log an apparent sea-level fall that is really rising shoreline. Beyond the former ice margin, on the forebulge, returning mantle drives the ground down, so relative sea level there outpaces the global average.
难度 进阶 · 适合 大众 CC BY 4.0 · 已核验 · Verified 2026-11-02
来源 · Source

Peltier 2004 年发表于《Annual Review of Earth and Planetary Sciences》的冰期地球均衡与ICE-5G模型研究

W. R. Peltier, Global glacial isostasy and the surface of the ice-age Earth: the ICE-5G (VM2) model and GRACE, Annual Review of Earth and Planetary Sciences, 2004

#冰后回弹 #相对海平面