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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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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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Thermal Energy Microscopically, thermal energy is the kinetic energy associated with the random motion of atoms and molecules. Temperature is a quantitative measure of “hot” or “cold”, which depends on the amount of thermal energy. When the atoms and molecules in an object are moving or vibrating quickly, they have a higher average kinetic energy (KE) (or higher thermal energy), and the object is perceived as “hot”, or it is described as being at a...
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A thermometer measures body temperature. The common sites for measuring body temperature are the oral cavity, axillary region, temporal artery, and skin surface, such as the forehead, abdomen, and axilla. True core body temperature is assessed in the rectum, tympanic membrane, pulmonary artery, esophagus, and urinary bladder.
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Precipitation gravimetry is based on converting an analyte into a sparingly soluble precipitate, which is separated by filtration and weighed. An ideal precipitate should be pure, insoluble, of known composition, and easily filtered from the reaction mixture.
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基于可靠的运营天气预报的热浪归因.

Nicholas J Leach1,2, Christopher D Roberts3, Matthias Aengenheyster4,3

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人类活动使2021年太平洋西北热浪的可能性增加了8倍. 由于全球变暖,这种极端天气事件的风险每20年翻一番,影响了适应计划.

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科学领域:

  • 气候科学气候科学
  • 极端天气归因 极端天气归因

背景情况:

  • 2021年太平洋西北部热浪的强度挑战了传统的极端天气归因方法.
  • 传统的统计和气候模型很难完全捕捉事件的物理.

研究的目的:

  • 量化人类引起的气候变化对2021年太平洋西北地区热浪的影响.
  • 评估在持续的全球变暖下,类似的极端热情事件的未来可能性.

主要方法:

  • 利用最先进的运营天气预报系统来模拟热浪的详细物理.
  • 利用这些模拟来进行基于预测的归因分析.

主要成果:

  • 人类的影响使2021年太平洋西北地区的热浪至少增加了8倍 (有95%的置信区间为2至50倍).
  • 按照目前的全球变暖速度,这种事件的可能性预计每20年翻一番 (95% CI: 10-50年).
  • 基于预测的归因为理解极端事件风险提供了一种综合方法.

结论:

  • 人为引起的气候变化显著增加了极端热情事件的可能性,例如2021年太平洋西北热浪.
  • 事件可能性的快速增加需要紧急考虑气候变化适应规划.
  • 开发基于预测的常规归因服务对于估计极端天气中的气候变化风险至关重要.