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Global Climate Change01:50

Global Climate Change

26.6K
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.
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What is Climate?01:16

What is Climate?

19.4K
Climate refers to the prevailing weather conditions in a specific area over an extended period. As the saying goes, “Climate is what you expect. Weather is what you get.” Climate is influenced by geographic factors, such as latitude, terrain, and proximity to bodies of water.
19.4K
What is Weather?01:07

What is Weather?

18.7K
Overview
18.7K
Precipitation Processes01:12

Precipitation Processes

1.4K
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...
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Influence of Earth's Curvature and Atmospheric Refraction on Leveling01:26

Influence of Earth's Curvature and Atmospheric Refraction on Leveling

405
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.
405
The Carbon Cycle01:14

The Carbon Cycle

42.2K
Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
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Related Experiment Video

Updated: Oct 27, 2025

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

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Observational evidence that cloud feedback amplifies global warming.

Paulo Ceppi1,2, Peer Nowack3,2,4,5

  • 1Grantham Institute, Imperial College London, London SW7 2AZ, United Kingdom; p.ceppi@imperial.ac.uk.

Proceedings of the National Academy of Sciences of the United States of America
|July 20, 2021
PubMed
Summary
This summary is machine-generated.

Global warming

Keywords:
climate changeclimate feedbacksclimate modelingclimate sensitivityclouds

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Area of Science:

  • Climate science
  • Earth system science
  • Atmospheric physics

Background:

  • Global warming alters Earth's cloud cover, influencing climate feedback loops.
  • Cloud feedback is the primary source of uncertainty in Equilibrium Climate Sensitivity (ECS).

Purpose of the Study:

  • To analyze cloud response to environmental changes using statistical learning.
  • To constrain global cloud feedback and its impact on climate sensitivity.

Main Methods:

  • Statistical learning analysis of Earth observation and climate model data.
  • Focusing on cloud sensitivity to surface temperature and tropospheric stability.

Main Results:

  • Global cloud feedback is primarily driven by surface temperature and tropospheric stability.
  • Constrained global cloud feedback: 0.43 ± 0.35 W⋅m⁻²⋅K⁻¹ (90% confidence).
  • A robustly amplifying effect of clouds on global warming is indicated.

Conclusions:

  • Low probability (0.5%) of Equilibrium Climate Sensitivity below 2 K.
  • The approach offers tighter constraints for climate change projections and impact assessments.