过去,现在和未来的进化,奥罗拉的亚冰川盆地的亚冰川排水系统
Anna-Mireilla Hayden1, Tyler Pelle2, Christine F Dow3
1Department of Geography and Environmental Management, University of Waterloo, Waterloo, Ontario, Canada. ahayden@uwaterloo.ca.
Nature communications
|March 21, 2025
概括
南极洲奥罗拉低冰盆地的冰下排水对冰流和质量损失产生了重大影响. 过去的模型忽略了这一点,但新的研究表明它在预测未来冰架融化和海平面上升方面发挥着至关重要的作用.
科学领域:
- 冰川学的冰川学
- 气候科学 气候科学
- 地球系统科学 地球系统科学
背景情况:
- 南极东部的奥罗拉亚冰川盆地 (ASB) 正在经历快速变化.
- 在ASB下方的冰下排水网络推动了快速的冰流和沿海冰架侵蚀,导致了质量损失.
- 过去的ASB前进-后退周期用于未来冰的行为预测,但往往忽视了冰下排水效应.
研究的目的:
- 模拟亚冰川排水网络的演变和冰架基底融化的ASB.
- 研究这些过程从3400万年前到公元2100年.
- 评估亚冰川水文学对南极冰块质量损失的影响.
主要方法:
- 冰下排水系统的数值建模.
- 模拟冰架基础融化的模拟.
- 古冰川学重建和未来预测.
主要成果:
- 数百万年来,ASB排水系统和冰架融化模式的持续重组.
- 证据表明,过去的冰动态并不是未来行为的完整模拟.
- 被确定为主要驱动因素的冰下排水,占冰架融化的70%左右.
结论:
- 亚冰川水文学在调节冰架融化和南极冰块质量损失方面发挥着关键作用.
- 未来的冰损失率可能比以前估计的要高,因为没有考虑冰下排水动态.
- 了解冰下过程对于准确的气候变化影响评估至关重要.
更多相关视频
13:38Laser-Induced Fluorescence Emission L.I.F.E. as Novel Non-Invasive Tool for In-Situ Measurements of Biomarkers in Cryospheric Habitats
Published on: October 26, 2019
7.9K
07:58Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt
Published on: August 7, 2017
9.3K
相关概念视频
Gradually Varying Flow
24
Gradually varying flow (GVF) in open channels describes situations where water depth changes slowly along the channel due to factors like non-uniform bed slope, channel shape variations, or obstructions. This flow type occurs when the depth adjusts gradually to balance gravitational forces, shear forces, and energy requirements, resulting in a low rate of depth change.Characteristics of Gradually Varying FlowGVF is commonly observed in natural streams, rivers, and canals, where flow depth...
24
Filtration and Urine Formation
49.0K
The function of the kidneys is to filter, reabsorb, secrete, and excrete. Every day the kidneys filter nearly 180 liters of blood, initially removing water and solutes but ultimately returning nearly all filtrates into circulation with the help of osmoregulatory hormones. This process removes wastes and toxins but is also crucial to maintain water and electrolyte levels. Most of these functions are performed by the tiny but numerous nephrons contained within the kidneys.
49.0K
Formation of Dilute Urine
1.2K
The formation of dilute urine is a critical renal adaptation that maintains fluid balance, particularly during periods of high fluid intake. This process primarily involves the juxtamedullary nephrons. By adjusting the permeability of water and ions in response to physiological conditions, the kidneys can either conserve or excrete water, resulting in concentrated or dilute urine.
Filtrate Osmolarity in the PCT
Initially, as the filtrate passes through the proximal convoluted tubule (PCT), its...
Filtrate Osmolarity in the PCT
Initially, as the filtrate passes through the proximal convoluted tubule (PCT), its...
1.2K
Formation of Concentrated Urine
1.2K
There is a gradient of solutes in the interstitial fluid from the renal cortex through the medulla, known as the medullary osmotic gradient. The juxtamedullary nephrons establish and maintain this gradient using countercurrent mechanisms with loops extending deep into the medulla. These nephrons also use countercurrent mechanisms to regulate urine volume and concentration. The interaction between the descending and ascending limbs of the nephron loop creates an osmotic gradient through...
1.2K
Veins of Lower Limbs
493
The human body consists of an intricate network of veins responsible for the crucial task of blood drainage from the lower limbs. These veins can be categorized into two main types: deep veins and superficial veins.
Formed by the union of the medial and lateral plantar veins, the posterior tibial vein, rising through the calf muscle, assimilates the fibular vein. The anterior tibial vein, a superior extension of the foot's dorsalis pedis vein, merges with the posterior tibial vein at the...
Formed by the union of the medial and lateral plantar veins, the posterior tibial vein, rising through the calf muscle, assimilates the fibular vein. The anterior tibial vein, a superior extension of the foot's dorsalis pedis vein, merges with the posterior tibial vein at the...
493
Global Climate Change
24.0K
Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
24.0K
