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Related Concept Videos

Precipitation Processes01:12

Precipitation Processes

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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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Global Climate Change01:50

Global Climate Change

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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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Precipitation and Co-precipitation01:17

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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...
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What is Climate?01:16

What is Climate?

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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.
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Boundary Layer Characteristics01:18

Boundary Layer Characteristics

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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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Types of Coprecipitation01:10

Types of Coprecipitation

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Coprecipitation is the contamination of a precipitate by otherwise soluble species and occurs via different processes. In colloidal precipitates, coprecipitation occurs via surface adsorption. For instance, barium sulfate has a primary layer of adsorbed barium ions and a secondary layer of nitrate counterions. This results in contamination of the precipitate by barium nitrate.
Sometimes, ions in a crystal lattice can undergo isomorphous replacement by inclusions of similar charge and size. For...
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Recent Advances in Understanding Multi-scale Climate Variability of the Asian Monsoon.

Wen Chen1,2, Renhe Zhang3, Renguang Wu4

  • 1Department of Atmospheric Sciences, Yunnan University, Kunming, 650500 China.

Advances in Atmospheric Sciences
|June 26, 2023
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Summary

Asian monsoon variability is crucial for global climate understanding. Recent studies reveal synchronized monsoon onsets, record rainfall events, and the influence of Arctic Oscillation and South Asian warming on monsoon recovery.

Keywords:
Asian monsoonEast Asian summer monsoonEast Asian winter monsoonIndian summer monsoonmonsoon onsetmulti-scale climate variability

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Area of Science:

  • Climate Science
  • Meteorology
  • Atmospheric Physics

Background:

  • The Asian monsoon system's multi-scale variability is critical for global climate system understanding.
  • Systematic review of recent advancements in Asian monsoon research is needed.

Purpose of the Study:

  • To systematically review progress in understanding Asian monsoon variability over recent years.
  • To highlight new findings concerning monsoon onset, East Asian and Indian monsoons, and their drivers.

Main Methods:

  • Literature review and synthesis of recent studies.
  • Analysis of observational data and climate model outputs (implied).
  • Focus on multi-scale processes influencing monsoon dynamics.

Main Results:

  • Synchronized local monsoon onset across the Arabian Sea, Bay of Bengal, Indochina, and South China Sea.
  • Detailed investigation of the 2020 record-breaking 'mei-yu' phenomenon and its multi-scale drivers.
  • East Asian winter monsoon recovery post-2000s, influenced by internal variability (Arctic Oscillation).
  • Accelerated South Asian warming driving Indian summer monsoon rainfall recovery since 1999.

Conclusions:

  • Recent research has significantly advanced the understanding of Asian monsoon variability.
  • Internal climate variability and regional warming are key drivers of observed monsoon changes.
  • Further research is needed to fully elucidate complex Asian monsoon dynamics.