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Global Climate Change01:50

Global Climate Change

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.
What is Natural Selection?01:32

What is Natural Selection?

Natural selection is an evolutionary process in which individuals with survival-promoting traits reproduce at higher rates. These favorable traits become more common within a population or species. Naturally selected traits initially arise via random genetic mutations. In order for selection to occur, there must be variation within a population, the trait controlling the variation must be heritable, and there must be an evolutionary advantage for variation in the trait.The Theory of Natural...
Variation in Acceleration due to Gravity near the Earth's Surface01:20

Variation in Acceleration due to Gravity near the Earth's Surface

An object's apparent weight is its weight measured by a spring balance at its location. It is different from its true weight, the force with which the Earth pulls it, because of the Earth's rotation. Mathematically, an object's apparent weight equals its true weight minus the centripetal force that keeps it in a circular motion along with the Earth's surface every 24 hours.
The difference between the true and apparent weights is proportional to the square of the Earth's angular speed. Since the...
Precipitation Gravimetry01:03

Precipitation Gravimetry

Precipitation gravimetry is based on converting an analyte into a sparingly soluble precipitate, which is separated by filtration and weighed. An ideal precipitate should be pure, insoluble, of known composition, and easily filtered from the reaction mixture.
In determining nickel by gravimetric analysis, a precipitant of ethanolic dimethylglyoxime is added to a hot nickel salt solution. This is quickly followed by the dropwise addition of dilute ammonia solution until precipitation occurs. A...
Precipitation Processes01:12

Precipitation Processes

The experimental conditions in a gravimetric analysis should be optimized to maximize the particle size and purity of the obtained precipitate. Ideally, the concentration of the precipitating reagent should be low with effective stirring to maintain low relative supersaturation for the growth of large crystals. In homogeneous precipitation, the precipitant is slowly generated by a chemical reaction in the solution to avoid local reagent excesses. For example, urea decomposes gradually to...
Average Value on a Rectangle01:27

Average Value on a Rectangle

A snowfall map can represent how snow depth varies across a region, such as Colorado, over a fixed time period. Since different locations may receive different amounts of snow, the snowfall depth is described by a function of two variables. If f(x,y) represents the snow depth at a point in a rectangular region, then the average snowfall over the entire region is found by comparing the total accumulated snowfall with the area being measured.Total Snowfall over a RegionThe total snowfall over a...

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相关实验视频

Updated: Jul 10, 2026

Measuring and Mapping Patterns of Soil Erosion and Deposition Related to Soil Carbonate Concentrations Under Agricultural Management
08:09

Measuring and Mapping Patterns of Soil Erosion and Deposition Related to Soil Carbonate Concentrations Under Agricultural Management

Published on: September 12, 2017

格陵兰冰盖海拔的变化主要归因于积雪的变化.

McConnell1, Arthern, Mosley-Thompson

  • 1Desert Research Institute, University & Community College System of Nevada, Reno 89512, USA. jmcconn@dri.edu

Nature
|September 6, 2000
PubMed
概括

格陵兰冰盖78-88年的海拔变化是由积雪的变化驱动的,不超过自然气候波动. 长期监测冰盖的升高和积雪的积累对于理解质量变化至关重要.

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:

  • 冰盖对气候变化的反应显著影响未来的海平面上升.
  • 卫星数据显示格陵兰的冰盖高度的空间变化,但地球物理过程仍然不清楚.
  • 区分最近的冰盖变化与自然变化是必不可少的.

研究的目的:

  • 为了确定1978-88年间格陵兰南部冰盖的海拔变化.
  • 确定负责观察到的海拔变化的地质物理过程.
  • 评估最近的变化是否属于格陵兰的自然气候变化.

主要方法:

  • 利用了基于物理的火密度模型.
  • 使用12个高海拔冰核的数据重建了年度积雪量.
  • 将建模的海拔变化与同期的卫星测量进行了比较.

主要成果:

  • 建模的积累驱动的海拔变化与1978-88年的卫星观测结果非常接近.
  • 将观察到的海拔变化归因于积雪量的变化.
  • 较长的冰芯分析表明格陵兰冰盖在自然界限内的典型变化.

结论:

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Last Updated: Jul 10, 2026

Measuring and Mapping Patterns of Soil Erosion and Deposition Related to Soil Carbonate Concentrations Under Agricultural Management
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Measuring and Mapping Patterns of Soil Erosion and Deposition Related to Soil Carbonate Concentrations Under Agricultural Management

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Simulating Impacts of Ice Storms on Forest Ecosystems

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In Situ Soil Moisture Sensors in Undisturbed Soils

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  • 雪积累的变化是格陵兰冰盖在1978-88年的海拔变化的主要驱动因素.
  • 观察到的变化符合冰盖的长期自然变化.
  • 综合,长期测量冰盖表面的升高和积雪是必要的,以进行全面的质量平衡评估.