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Thermosensation01:43

Thermosensation

33.3K
Peripheral thermosensation is the perception of external temperature. A change in temperature (on the surface of the skin and other tissues) is detected by a family of temperature-sensitive ion channels called Transient Receptor Potential, or TRP, receptors. These receptors are located on free nerve endings. Those detecting cold temperatures are closer to the surface of the skin than the nerve endings detecting warmth. These thermoTRP channels, while temperature selective, have relatively...
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Precipitation Gravimetry01:03

Precipitation Gravimetry

11.7K
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.
In determining nickel by gravimetric analysis, a precipitant of ethanolic dimethylglyoxime is added to a hot nickel salt solution. This is quickly followed by the dropwise addition of dilute ammonia solution until precipitation occurs. A...
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Temperature Measurement Sites01:14

Temperature Measurement Sites

2.8K
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.
Oral: When assessing oral temperature, the thermometer tip should be placed under the tongue in the posterior sublingual pocket. It offers accurate readings and can be...
2.8K
Thermometers and Temperature Scales01:22

Thermometers and Temperature Scales

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Any physical property that depends consistently and reproducibly on temperature can be used as the basis of a thermometer. For example, volume increases with temperature for most substances. This property is the basis for the common alcohol thermometer and the original mercury thermometers. Other properties used to measure temperature include electrical resistance, color, and the emission of infrared radiation.
As many physical properties depend on temperature, the variety of thermometers is...
6.9K
Constant Pressure Calorimetry03:02

Constant Pressure Calorimetry

96.4K
Calorimetry is a technique used to measure the amount of heat involved in a chemical or physical process or to measure the heat transferred to or from a substance. The heat is exchanged with a calibrated and insulated device called the calorimeter. Calorimetry experiments are based on the assumption that there is no heat exchange between the insulated calorimeter and the external environment. The well-insulated calorimeters prevent the transfer of heat between the calorimeter and its external...
96.4K
Gas Thermometers and the Kelvin Scale01:22

Gas Thermometers and the Kelvin Scale

5.8K
The definition of temperature in terms of molecular motion suggests that there should be a lowest possible temperature, where the average kinetic energy of molecules is zero (or the minimum allowed by quantum mechanics). Experiments confirm the existence of such a temperature, called absolute zero. An absolute temperature scale is one whose zero point is absolute zero. Such scales are convenient in science because several physical quantities, such as the volume of an ideal gas, are directly...
5.8K

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Updated: Dec 8, 2025

Evolution of Staircase Structures in Diffusive Convection
07:28

Evolution of Staircase Structures in Diffusive Convection

Published on: September 5, 2018

6.8K

Termometría sísmica del océano

Wenbo Wu1, Zhongwen Zhan2, Shirui Peng2

  • 1Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA. wenbow@caltech.edu.

Science (New York, N.Y.)
|September 18, 2020
PubMed
Resumen
Este resumen es generado por máquina.

El calentamiento del océano se controla mediante la termometría sísmica del océano, que analiza las ondas sonoras generadas por un terremoto. Este método revela tendencias significativas de calentamiento decenal en el Océano Índico Oriental, que exceden las estimaciones anteriores.

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Author Spotlight: Unveiling Plankton Response to Climate Change Through Time-Series Data and Artistic Expression
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Área de la Ciencia:

  • La oceanografía
  • Sismología
  • Ciencias del clima

Sus antecedentes:

  • Los gases de efecto invernadero atrapan la energía, y los océanos absorben más del 90% de este calor.
  • El monitoreo del calentamiento de las profundidades oceánicas es difícil debido a la escasez de datos.
  • Los métodos existentes tienen dificultades para capturar los cambios de temperatura a escala de cuenca.

Objetivo del estudio:

  • Introducir un nuevo método para inferir los cambios de temperatura de las profundidades oceánicas a escala de cuenca.
  • Para complementar las mediciones tradicionales de la temperatura del océano basadas en puntos.
  • Para proporcionar una comprensión más completa de la dinámica del calentamiento del océano.

Principales métodos:

  • Utilizando ondas sonoras generadas por repetidos terremotos.
  • Aplicación de la termometría sísmica del océano para analizar los tiempos de viaje de las olas.
  • Anomalías de temperatura restrictivas en el Océano Índico oriental ecuatorial en una sección de 3000 km.

Principales resultados:

  • Anomalías de temperatura con un error estándar de 0,0060 grados Kelvin.
  • Fluctuaciones de temperatura detectadas en varias escalas de tiempo (12 meses, 6 meses, ~10 días).
  • Inferido una tendencia al calentamiento decenal significativamente mayor que las estimaciones anteriores.

Conclusiones:

  • La termometría sísmica del océano ofrece un método viable para monitorear el calentamiento de las profundidades oceánicas.
  • El estudio destaca el calentamiento sustancial y acelerado en el Océano Índico Oriental.
  • Los resultados subrayan la urgencia de abordar las emisiones de gases de efecto invernadero y su impacto en los océanos.