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関連する概念動画

Influence of Earth's Curvature and Atmospheric Refraction on Leveling01:26

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...
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...
Root Loci for Positive-Feedback Systems01:23

Root Loci for Positive-Feedback Systems

The Hartley oscillator is a positive feedback system that sustains oscillations by feeding the output back to the input in phase, thereby reinforcing the signal. Positive feedback systems can be viewed as negative feedback systems with inverted feedback signals. In these systems, the root locus encompasses all points on the s-plane where the angle of the system transfer function equals 360 degrees.
The construction rules for the root locus in positive feedback systems are similar to those in...
Positive and Negative Feedback Loops01:18

Positive and Negative Feedback Loops

Animal organs and organ systems constantly adjust to internal and external changes through a process called homeostasis ("steady state"). Examples of these changes include regulation of the level of glucose or calcium in the blood or internal responses to external temperatures. Homeostasis requires  maintaining an internal dynamic equilibrium:
Precipitation and Co-precipitation01:17

Precipitation and Co-precipitation

Precipitation and coprecipitation methods can be used to separate a mixture of ions in a solution. In qualitative inorganic analysis, ions that form sparingly soluble precipitates with the same reagent are separated based on the differences in solubility products. For example, consider the separation of Cu(II) and Fe(II) ions by precipitation as insoluble sulfides. First, copper(II) sulfide is precipitated by the addition of acidic H2S, where the dissociation of H2S is suppressed. Adding H2S...
Boundary Layer Characteristics01:18

Boundary Layer Characteristics

When a fluid encounters a solid surface, a boundary layer forms due to the interaction between the fluid's motion and the stationary surface. This phenomenon is characterized by a thin region adjacent to the surface where viscous forces dominate, influencing the fluid's velocity profile. The development of the boundary layer begins at the leading edge of the surface and evolves as the fluid moves downstream.As the fluid flows over the surface, friction between the fluid and the wall slows down...

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関連する実験動画

Updated: Jun 21, 2026

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
13:27

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface

Published on: June 8, 2015

ポジティブな低レベルのクラウドフィードバックの観測およびモデルの証拠

Amy C Clement1, Robert Burgman, Joel R Norris

  • 1Rosenstiel School of Marine and Atmospheric Sciences, University of Miami, Division of Meteorology and Physical Oceanography, MSC 362, 4600 Rickenbacker Causeway, Miami, FL 33149, USA. aclement@rsmas.miami.edu

Science (New York, N.Y.)
|July 25, 2009
PubMed
まとめ

低レベルの雲は,気候モデルに不確実性をもたらします. この研究では,観測された雲がポジティブなフィードバックとして作用することを発見し,これを支持する1つのモデルは,温室効果ガスの増加による雲の覆いの減少を示しています.

科学分野:

  • 大気科学 大気科学
  • 気候モデリング
  • 海洋-大気相互作用

背景:

  • 低レベルの雲は,世界の気候モデルの予測における不確実性の主要な源である.
  • 雲のフィードバックを理解することは,正確な気候変動の予測に不可欠です.

研究 の 目的:

  • 観測と気候モデルを使用して,北東太平洋上の低層雲の変化を調査する.
  • 現在の気候モデルにおける雲のシミュレーションの現実性をテストする.

主な方法:

  • 複数の独立した低レベルのクラウドデータセットにおける10年間の変動の分析.
  • 観測された雲の覆いの変化と,局所的な気温構造と,大規模な循環の相関.
  • 観測された雲-気象学的関係を再現する能力に基づく気候モデルの評価.

主要な成果:

  • 低レベルの雲の覆いにおける10年間の変動は,独立した観測データセットで特定されました.
  • 観測された雲の覆いの変化は,地域的な気温構造と大規模な大気循環と関連していた.
  • ある気候モデルでは,観測された関係を成功裏に再現し,温室効果ガスの増加下で太平洋の雲の覆いが減少したシミュレーションを行いました.

結論:

さらに関連する動画

Extraction and Characterization of Surfactants from Atmospheric Aerosols
09:34

Extraction and Characterization of Surfactants from Atmospheric Aerosols

Published on: April 21, 2017

Measurement of Aerosols Optical Thickness of the Atmosphere using the GLOBE Handheld Sun Photometer
06:27

Measurement of Aerosols Optical Thickness of the Atmosphere using the GLOBE Handheld Sun Photometer

Published on: May 29, 2019

関連する実験動画

Last Updated: Jun 21, 2026

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
13:27

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface

Published on: June 8, 2015

Extraction and Characterization of Surfactants from Atmospheric Aerosols
09:34

Extraction and Characterization of Surfactants from Atmospheric Aerosols

Published on: April 21, 2017

Measurement of Aerosols Optical Thickness of the Atmosphere using the GLOBE Handheld Sun Photometer
06:27

Measurement of Aerosols Optical Thickness of the Atmosphere using the GLOBE Handheld Sun Photometer

Published on: May 29, 2019

  • 観測結果によると,低層雲は,北東太平洋における10年間の時間スケールに対する肯定的なフィードバックとして作用している.
  • この研究は,雲のフィードバックに関する気候モデルのリアリズムをテストするための方法を提供します.
  • モデリングの証拠は,温暖化気候におけるポジティブな低レベルの雲のフィードバックメカニズムを示唆しています.