Jove
Visualize
Contáctanos
JoVE
x logofacebook logolinkedin logoyoutube logo
ACERCA DE JoVE
Visión GeneralLiderazgoBlogCentro de Ayuda JoVE
AUTORES
Proceso de PublicaciónConsejo EditorialAlcance y PolíticasRevisión por ParesPreguntas FrecuentesEnviar
BIBLIOTECARIOS
TestimoniosSuscripcionesAccesoRecursosConsejo Asesor de BibliotecasPreguntas Frecuentes
INVESTIGACIÓN
JoVE JournalMethods CollectionsJoVE Encyclopedia of ExperimentsArchivo
EDUCACIÓN
JoVE CoreJoVE BusinessJoVE Science EducationJoVE Lab ManualCentro de Recursos para ProfesoresSitio de Profesores
Términos y Condiciones de Uso
Política de Privacidad
Políticas

Videos de Conceptos Relacionados

What is Weather?01:07

What is Weather?

Overview
Precipitation Titration: Overview01:26

Precipitation Titration: Overview

Precipitation titration involves the reaction of a titrant and an analyte to generate an insoluble precipitate. While precipitation titration uses various precipitating agents, silver nitrate is the most common precipitating reagent; titrations involving Ag+ are called argentometric titrations. Usually, the endpoint in a precipitation titration can be detected by visual indicators.
A precipitation titration curve demonstrates the change in concentration of the titrant or analyte upon adding the...
Precipitation Gravimetry01:03

Precipitation Gravimetry

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...
Precipitation Processes01:12

Precipitation Processes

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...
Precipitation and Co-precipitation01:17

Precipitation and Co-precipitation

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...
Surface Integrals of Vector Fields: Flux01:22

Surface Integrals of Vector Fields: Flux

Understanding the movement of air masses is fundamental to meteorological analysis and atmospheric modeling. A key component in this process is quantifying the total mass of air that flows into or out of a defined region over a specified period of time. This is achieved by evaluating the mass flux across a boundary surface, a conceptual tool that simplifies the complex dynamics of atmospheric systems.To begin, an imaginary boundary surface S is introduced, enclosing the region of interest. The...

También podría leer

Artículos Relacionados

Artículos vinculados a este trabajo por autores compartidos, revista y gráfico de citas.

Ordenar por
Same author

Comparing variable selection and model averaging methods for logistic regression.

Proceedings of the National Academy of Sciences of the United States of America·2026
Same author

Bringing Age Back In: Accounting for Population Age Distribution in Forecasting Migration.

Demography·2026
Same author

Bayesian Projection of Extant Refugee and Asylum Seeker Populations.

Demography·2025
Same author

Author Correction: Optimal pandemic control strategies and cost-effectiveness of COVID-19 non-pharmaceutical interventions in the United States.

BMC global and public health·2025
Same author

Mitigation efforts to reduce carbon dioxide emissions and meet the Paris Agreement have been offset by economic growth.

Communications earth & environment·2025
Same author

Optimal pandemic control strategies and cost-effectiveness of COVID-19 non-pharmaceutical interventions in the United States.

BMC global and public health·2025

Video Experimental Relacionado

Updated: Jul 11, 2026

Surface Renewal: An Advanced Micrometeorological Method for Measuring and Processing Field-Scale Energy Flux Density Data
09:55

Surface Renewal: An Advanced Micrometeorological Method for Measuring and Processing Field-Scale Energy Flux Density Data

Published on: December 12, 2013

Ciencias de la atmósfera. ciencia atmosférica. Pronóstico del tiempo con métodos de conjunto.

Tilmann Gneiting1, Adrian E Raftery

  • 1Department of Statistics, University of Washington, Box 354322, Seattle, WA 98195, USA. tilmann@stat.washington.edu

Science (New York, N.Y.)
|October 15, 2005
PubMed
Resumen

El pronóstico conjunto utiliza múltiples ejecuciones de computadoras para predecir el clima, ofreciendo mejores estimaciones de incertidumbre que los métodos tradicionales. Mejorar el modelado y la difusión de conjuntos es clave para la precisión futura.

Más Videos Relacionados

Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information
10:28

Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information

Published on: June 13, 2020

Generation of Dynamical Environmental Conditions using a High-Throughput Microfluidic Device
14:48

Generation of Dynamical Environmental Conditions using a High-Throughput Microfluidic Device

Published on: April 17, 2021

Videos de Experimentos Relacionados

Last Updated: Jul 11, 2026

Surface Renewal: An Advanced Micrometeorological Method for Measuring and Processing Field-Scale Energy Flux Density Data
09:55

Surface Renewal: An Advanced Micrometeorological Method for Measuring and Processing Field-Scale Energy Flux Density Data

Published on: December 12, 2013

Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information
10:28

Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information

Published on: June 13, 2020

Generation of Dynamical Environmental Conditions using a High-Throughput Microfluidic Device
14:48

Generation of Dynamical Environmental Conditions using a High-Throughput Microfluidic Device

Published on: April 17, 2021

Área de la Ciencia:

  • Meteorología Meteorología.
  • Ciencias atmosféricas Ciencias atmosféricas.
  • Ciencias del clima Ciencias del clima Ciencias del clima Ciencias del clima

Sus antecedentes:

  • El pronóstico del tiempo tradicional se basa en modelos deterministas, proporcionando predicciones únicas basadas en las condiciones iniciales.
  • Los modelos deterministas tienen limitaciones para capturar la incertidumbre inherente de los sistemas atmosféricos.

Objetivo del estudio:

  • Introducir y explicar el concepto de pronóstico de conjuntos como un avance sobre los métodos deterministas.
  • Para resaltar los beneficios del pronóstico conjunto en la cuantificación de la incertidumbre en las predicciones meteorológicas.

Principales métodos:

  • La predicción de conjuntos implica ejecutar múltiples simulaciones (ensembles) con condiciones iniciales o parámetros de modelo variados.
  • Las técnicas estadísticas se integran con los resultados del conjunto para analizar e interpretar la incertidumbre de los pronósticos.

Principales resultados:

  • Los pronósticos conjuntos proporcionan declaraciones más precisas sobre la incertidumbre en las predicciones meteorológicas diarias y estacionales.
  • Este enfoque permite una comprensión probabilística de los resultados futuros del clima.

Conclusiones:

  • El pronóstico conjunto representa un cambio significativo desde el modelado determinista en meteorología.
  • Se necesitan avances adicionales en el modelado, el análisis estadístico y la visualización para optimizar la difusión del pronóstico conjunto.