SAGE衛星システムによって測定されたSoufriere火山からのストラトスフィアのエアロゾール効果
まとめ
ソフリエール火山 (Soufriere Volcano) とは
科学分野:
- 火山学 火山学とは
- 大気科学 大気科学
- 気候科学 気候科学
背景:
- 1979年4月のソフリエール火山の噴火は,重要な平流層の羽根を生成しました.
- 火山噴火による大気への影響を理解することは,気候モニタリングに不可欠です.
研究 の 目的:
- 1979年のソフリエール噴火からの平流層の羽根の軌跡と分散を追跡するために.
- これらの羽根が地球上の平流層のエアロゾール負荷と気候に与える潜在的な影響を評価する.
主な方法:
- ストラトスフィア・エアロゾール・アンド・ガス・エクスペリメント (SAGE) 衛星システムからのデータを活用した.
- 気象データと確立された分散理論を用いて,羽根の移動と分散を分析した.
主要な成果:
- 2つの主要な平流層の羽根が特定され,西アフリカと北大西洋に向かって追跡されました.
- 火山噴火の総質量は,地球上の平流圏のエアロゾール負荷の0.5%未満を占めています.
結論:
- 羽根の移動と分散は,気象データと分散モデルと一致していました.
- ストラトスフィアに注入される火山性エアロゾールの質量が限られているため,気温や気候の変動は予想されません.
関連する概念動画
The Sulfur Cycle
Sulfur, an important element in the chemical makeup of proteins, is recycled through the atmosphere and aquatic and terrestrial environments. Found in the atmosphere as sulfur dioxide (SO2), sulfur is released by decaying organisms, weathered rocks, geothermal vents, volcanos, and burning fossil fuels. It is deposited into the ecosystem, cycled through the biotic community, and either released back into the atmosphere as gas or deposited in marine sediment for long-term storage and eventual...
Influence of Earth's Curvature and Atmospheric Refraction on Leveling
During leveling, the Earth's curvature and atmospheric refraction introduce deviations in the line of sight from a true horizontal reference. When the line of sight is leveled, it remains perpendicular to the plumb line only at a single point. Beyond this, it deviates due to the Earth’s curvature, represented by the correction C. For a sight distance D, the deviation can be derived using the relationship:This relationship shows that the deviation increases quadratically with distance. Over a...
Sulfur Assimilation
Sulfur is an essential element in biological systems, contributing to synthesizing key biomolecules, including amino acids such as cysteine and methionine, and cofactors such as coenzyme A and biotin. Microorganisms primarily assimilate sulfur as sulfate (SO₄²⁻) from the environment, which must undergo a series of biochemical transformations before it can be incorporated into cellular components. As sulfate is highly oxidized, it must undergo assimilatory sulfate reduction to become...
Atomic Spectroscopy: Effects of Temperature
Atomization, converting samples into gas-phase atoms and ions, is essential for atomic spectroscopy. The flame temperature required for atomization affects the efficiency of the atomic spectroscopic methods by increasing the atomization efficiency and the relative population of the excited and ground states.
At thermal equilibrium, the relative populations of excited and ground state atoms can be estimated using the Maxwell–Boltzmann distribution. For example, an increase in temperature from...
At thermal equilibrium, the relative populations of excited and ground state atoms can be estimated using the Maxwell–Boltzmann distribution. For example, an increase in temperature from...
Attenuated Total Reflectance (ATR) Infrared Spectroscopy: Overview
Attenuated total reflectance (ATR) infrared spectroscopy is a powerful analytical technique used to study the composition of materials. It is widely employed in chemistry, materials science, forensic science, and other fields where sample characterization is required. ATR has several advantages over traditional transmission IR spectroscopy, including the requirement of little to no sample preparation and the ability to analyze a wide range of samples.
The ATR process begins by directing a beam...
The ATR process begins by directing a beam...
Variation of Atmospheric Pressure
Change in atmospheric pressure with height is particularly interesting. The decrease in atmospheric pressure with increasing altitude is due to the decreasing gravitational force per unit area as we move away from the surface of the earth.
Assuming the air temperature is constant at a given altitude and that the ideal gas law of thermodynamics describes the atmosphere to a good approximation, one can find the variation of atmospheric pressure with height.
Let p(y) be the atmospheric pressure at...
Assuming the air temperature is constant at a given altitude and that the ideal gas law of thermodynamics describes the atmosphere to a good approximation, one can find the variation of atmospheric pressure with height.
Let p(y) be the atmospheric pressure at...


