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The relative frequency depicts the proportion of data points that have each value. The frequency tells the number of data points that have each value. Like the histogram, a relative frequency histogram also has the same shape with a horizontal scale (the x-axis), but the vertical scale (the y-axis) is marked with relative frequencies (percentages of the whole) instead of actual frequencies. A relative frequency histogram is a graphical representation of a frequency distribution where the...
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A time-series graph is a line graph with repeated measurements taken at successive intervals of time. It is also called a time series chart. To construct a time-series graph, one must look at both pieces of a paired data set. The horizontal axis is used to plot the time increments, and the vertical axis is used to plot the values of the variable that one is measuring. By using the axes in this way, each point on the graph will correspond to time and a measured quantity. The points on the graph...
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Run charts, essentially line graphs plotted over time, serve as fundamental yet effective tools for process analysis. They chronicle data sequentially, facilitating the identification of trends, shifts, or cyclical movements. This graphical representation is instrumental in determining whether a process is stable or exhibits signs of potential instability indicative of special cause variation. In the healthcare domain, run charts depict infection rates over time, enabling hospitals to monitor...
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Video Experimental Relacionado

Updated: Jul 6, 2026

Tracking Infiltration Front Depth Using Time-lapse Multi-offset Gathers Collected with Array Antenna Ground Penetrating Radar
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Tendencias temporales en las profundidades del océano Las relaciones de Redfield.

M Pahlow1, U Riebesell

  • 1Alfred Wegener Institute for Polar and Marine Research, Post Office Box 120161, D-27515 Bremerhaven, Germany. mpahlow@awi-bremerhaven.de

Science (New York, N.Y.)
|February 5, 2000
PubMed
Resumen

El ciclo del carbono marino está cambiando. Las proporciones de flujo de partículas del océano profundo (carbono: nitrógeno: fósforo) muestran tendencias temporales, lo que indica que la bomba de carbono biológica no está en estado estacionario.

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Área de la Ciencia:

  • Biogeoquímica marina y biogeoquímica marina.
  • Oceanografía La oceanografía es la oceanografía.
  • Ciencias del clima Ciencias del clima Ciencias del clima

Sus antecedentes:

  • La relación Redfield (carbono: nitrógeno: fósforo) es crucial para el ciclo biogeoquímico marino y el secuestro de carbono.
  • Esta relación se asume típicamente constante en el océano moderno, pero los datos recientes sugieren lo contrario.

Objetivo del estudio:

  • Para investigar las tendencias temporales en las relaciones de Redfield de aguas profundas en el hemisferio norte durante las últimas cinco décadas.
  • Comprender las implicaciones de estas tendencias para el ciclo y el secuestro de carbono marino.

Principales métodos:

  • Análisis de datos de flujo de partículas de aguas profundas de los océanos Atlántico Norte y Pacífico Norte.
  • Correlación de los cambios en la relación de Redfield con factores potenciales como la deposición atmosférica y las condiciones oceanográficas.

Principales resultados:

  • El Atlántico Norte muestra un aumento de la proporción nitrógeno: fósforo, potencialmente vinculado a las emisiones antropogénicas de óxido nitroso.
  • El Pacífico Norte exhibe crecientes proporciones de carbono: nitrógeno y carbono: fósforo, asociadas con el aumento de las tasas de remineralización y la intensificación de la producción de exportación.
  • El aumento de la biodisponibilidad del hierro eólico puede estar impulsando el aumento de las exportaciones de carbono en el Pacífico Norte.

Conclusiones:

  • Las proporciones de Redfield en aguas profundas en el hemisferio norte no son constantes y muestran tendencias temporales significativas.
  • Estos cambios sugieren que la bomba de carbono biológica no se encuentra actualmente en un estado estacionario.
  • Los hallazgos tienen implicaciones para la comprensión del secuestro de carbono oceánico y su respuesta a las influencias antropogénicas.