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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.
Carbon Dioxide Transport in the Blood01:19

Carbon Dioxide Transport in the Blood

Carbon dioxide (CO2) transport in the blood is critical to human physiology. On average, our body cells produce around 200 mL of CO2 per minute, precisely the quantity expelled by the lungs. This process involves the transportation of CO2 from the tissue cells to the lungs in three primary forms.
Forms of CO2 Transport
1. Dissolved in plasma: A small percentage (7-10%) of CO2 is transported and dissolved directly in the plasma.
2. Carbaminohemoglobin: Just over 20% of CO2 is chemically bound to...
Chemical Factors Affecting Respiration Centers01:31

Chemical Factors Affecting Respiration Centers

Chemical factors such as changing CO2, O2, and H+ levels in arterial blood play a critical role in influencing respiration depth and rates. These variations are detected by chemoreceptors—specialized sensors located in two primary body areas. Central chemoreceptors are found throughout the brain stem, including the ventrolateral medulla, while peripheral chemoreceptors are located in the aortic arch and carotid arteries.
CO2 has a potent influence on respiration and is strictly regulated. Under...
Oxygen Transport in the Blood01:27

Oxygen Transport in the Blood

Hemoglobin (Hb) is a crucial molecule in the human body, consisting of four polypeptide chains, each bound to an iron-containing heme group. This unique structure enables hemoglobin to bind to oxygen, with each molecule capable of combining with four molecules of oxygen, leading to rapid and reversible oxygen loading. When fully loaded with oxygen, it is called oxyhemoglobin, while hemoglobin that has released oxygen is called reduced hemoglobin or deoxyhemoglobin. As hemoglobin binds oxygen,...
Assessment of Diffusion and Perfusion01:17

Assessment of Diffusion and Perfusion

Understanding and evaluating diffusion and perfusion is critical in assessing a patient's respiratory and circulatory health. These processes play key roles in maintaining the body's internal environment, ensuring that tissues receive adequate oxygen while waste products are efficiently removed.
The Role of Diffusion in Respiration
Diffusion is the process by which molecules move from an area of higher concentration to an area of lower concentration. In the respiratory system, this principle...
Variation of Atmospheric Pressure01:18

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...

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関連する実験動画

Updated: Jul 12, 2026

Split Point Analysis and Uncertainty Quantification of Thermal-Optical Organic/Elemental Carbon Measurements
10:22

Split Point Analysis and Uncertainty Quantification of Thermal-Optical Organic/Elemental Carbon Measurements

Published on: September 7, 2019

大気中の一酸化炭素の最近の変化

P C Novelli, K A Masarie, P P Tans

    Science (New York, N.Y.)
    |March 18, 1994
    PubMed
    まとめ

    大気中の一酸化炭素 (CO) レベルは,過去2~5年間にわたって世界的に減少しており,これは以前の長期増加から大きく反転しています. この研究は,異なる半球と緯度におけるCO減少の速度を詳細に説明しています.

    科学分野:

    • 大気化学 大気化学
    • 環境科学 環境科学
    • 気候変動研究 気候変動研究

    背景:

    • 長期の大気測定は,過去30年間にわたって,特に北半球で,一酸化炭素 (CO) の濃度が増加する歴史的な傾向を示しています.
    • 以前の研究では,北半球のデータに基づいて,CO濃度の年間1~2%の増加を推論していた.

    研究 の 目的:

    • 最近の世界的な大気中の一酸化炭素 (CO) の動向を分析する.
    • 世界中のCO濃度変化の空間的および時間的変動を特定するために.
    • 現在のCOトレンドを過去の長期データと比較する.

    主な方法:

    • 北緯71度から南緯41度までの27の異なる地理的な場所から採取された空気サンプルを分析した.
    • 採取した空気サンプルにおける一酸化炭素 (CO) 濃度の定量測定.
    • CO濃度のデータを統計的に分析して,特定の期間 (過去2~5年) における変化率を特定し,過去の傾向と比較する.

    主要な成果:

    • 大気中の一酸化炭素 (CO) 濃度が過去2~5年間に世界中で減少していることが観察されました.
    • COは,高北緯度ではほぼ恒常的な減少率を示した.
    • 1991年後半から熱帯では急激なCO2減少が観測されました.

    さらに関連する動画

    Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.
    07:32

    Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.

    Published on: June 4, 2021

    Fa&#231;ade-Level Monitoring of CO2 Variability under Urban Heat Island Conditions using Low-Cost Sensor Data Loggers
    07:12

    Façade-Level Monitoring of CO2 Variability under Urban Heat Island Conditions using Low-Cost Sensor Data Loggers

    Published on: December 12, 2025

    関連する実験動画

    Last Updated: Jul 12, 2026

    Split Point Analysis and Uncertainty Quantification of Thermal-Optical Organic/Elemental Carbon Measurements
    10:22

    Split Point Analysis and Uncertainty Quantification of Thermal-Optical Organic/Elemental Carbon Measurements

    Published on: September 7, 2019

    Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.
    07:32

    Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.

    Published on: June 4, 2021

    Fa&#231;ade-Level Monitoring of CO2 Variability under Urban Heat Island Conditions using Low-Cost Sensor Data Loggers
    07:12

    Façade-Level Monitoring of CO2 Variability under Urban Heat Island Conditions using Low-Cost Sensor Data Loggers

    Published on: December 12, 2025

  • 北半球では1990年6月から1993年6月まで,平均COの減少が7.3 (+/-0.9) ppb/年 (6.1%/年) であった.
  • 南半球では,平均CO2の減少が4.2 (+/-0.5) ppb/年 (7.0%/年) であった.
  • 結論:

    • 最近の世界の大気中のCO2レベルは,長期にわたる増加傾向を逆転させました.
    • 観測されたCO減少は,大気化学または排出源の最近の重要な変化を示唆しています.
    • 半球と緯度間のCO減少の異なるパターンは,地域の大気過程のさらなる調査を正当化します.