Jove
Visualize
Contact Us
JoVE
x logofacebook logolinkedin logoyoutube logo
ABOUT JoVE
OverviewLeadershipBlogJoVE Help Center
AUTHORS
Publishing ProcessEditorial BoardScope & PoliciesPeer ReviewFAQSubmit
LIBRARIANS
TestimonialsSubscriptionsAccessResourcesLibrary Advisory BoardFAQ
RESEARCH
JoVE JournalMethods CollectionsJoVE Encyclopedia of ExperimentsArchive
EDUCATION
JoVE CoreJoVE BusinessJoVE Science EducationJoVE Lab ManualFaculty Resource CenterFaculty Site
Terms & Conditions of Use
Privacy Policy
Policies

Related Concept Videos

Mechanistic Models: Compartment Models in Algorithms for Numerical Problem Solving01:29

Mechanistic Models: Compartment Models in Algorithms for Numerical Problem Solving

41
Mechanistic models play a crucial role in algorithms for numerical problem-solving, particularly in nonlinear mixed effects modeling (NMEM). These models aim to minimize specific objective functions by evaluating various parameter estimates, leading to the development of systematic algorithms. In some cases, linearization techniques approximate the model using linear equations.
In individual population analyses, different algorithms are employed, such as Cauchy's method, which uses a...
41
Estimation of the Physical Quantities01:05

Estimation of the Physical Quantities

4.2K
On many occasions, physicists, other scientists, and engineers need to make estimates of a particular quantity. These are sometimes referred to as guesstimates, order-of-magnitude approximations, back-of-the-envelope calculations, or Fermi calculations. The physicist Enrico Fermi was famous for his ability to estimate various kinds of data with surprising precision. Estimating does not mean guessing a number or a formula at random. Instead, estimation means using prior experience and sound...
4.2K
Influence of Earth's Curvature and Atmospheric Refraction on Leveling01:26

Influence of Earth's Curvature and Atmospheric Refraction on Leveling

54
During leveling, the Earth's curvature and atmospheric refraction introduce deviations in the line of sight from a true horizontal reference. When the line of sight is leveled, it remains perpendicular to the plumb line only at a single point. Beyond this, it deviates due to the Earth’s curvature, represented by the correction C. For a sight distance D, the deviation can be derived using the relationship:This relationship shows that the deviation increases quadratically with distance.
54
Stability of Equilibrium Configuration01:23

Stability of Equilibrium Configuration

433
Understanding the stability of equilibrium configurations is a fundamental part of mechanical engineering. In any system, there are three distinct types of equilibrium: stable, neutral, and unstable.
A stable equilibrium occurs when a system tends to return to its original position when given a small displacement, and the potential energy is at its minimum. An example of a stable equilibrium is when a cantilever beam is fixed at one end and a weight is attached to the other end. If the weight...
433
Equilibrium Conditions for a Particle01:23

Equilibrium Conditions for a Particle

1.0K
When an object is in equilibrium, it is either at rest or moving with a constant velocity. There are two types of equilibrium: static and dynamic. Static equilibrium occurs when an object is at rest, while dynamic equilibrium occurs when an object is moving with a constant velocity. In both cases, there must be a balance of forces acting on the object.
To understand the concept of equilibrium, let us first consider the forces acting on an object. When different forces act on an object, they can...
1.0K
Equations of Equilibrium in Three Dimensions01:30

Equations of Equilibrium in Three Dimensions

1.1K
When analyzing structures or systems at rest, it is necessary to ensure they are in equilibrium. This is where the vector and scalar equations of equilibrium come into play. These equations are crucial in ensuring a structure is stable and will not collapse or fall apart. The vector and scalar equations of equilibrium provide a framework for analyzing the forces acting on a body.
According to the vector equations of equilibrium, the vector sum of all the external forces acting on a body must...
1.1K

You might also read

Related Articles

Articles linked to this work by shared authors, journal, and citation graph.

Sort by
Same author

More extreme Indian monsoon rainfall in El Niño summers.

Science (New York, N.Y.)·2025
Same author

A mutual information criterion with applications to canonical correlation analysis and graphical models.

Stat (International Statistical Institute)·2021
Same author

Standard assessments of climate forecast skill can be misleading.

Nature communications·2021
Same author

Monthly ENSO Forecast Skill and Lagged Ensemble Size.

Journal of advances in modeling earth systems·2018
Same author

The Weighted-Average Lagged Ensemble.

Journal of advances in modeling earth systems·2018
Same author

A new method for determining the optimal lagged ensemble.

Journal of advances in modeling earth systems·2017
Same journal

A New Aerosol Dry Deposition Model for Air Quality and Climate Modeling.

Journal of advances in modeling earth systems·2025
Same journal

BioRT-HBV 1.0: A Biogeochemical Reactive Transport Model at the Watershed Scale.

Journal of advances in modeling earth systems·2024
Same journal

Accurate and Efficient Numerical Simulation of Land Models Using SUMMA With SUNDIALS.

Journal of advances in modeling earth systems·2024
Same journal

Reconstructing the Tropical Pacific Upper Ocean Using Online Data Assimilation With a Deep Learning Model.

Journal of advances in modeling earth systems·2024
Same journal

Estimating Ocean Heat Uptake Using Boundary Green's Functions: A Perfect-Model Test of the Method.

Journal of advances in modeling earth systems·2023
Same journal

Deep Learning Based Cloud Cover Parameterization for ICON.

Journal of advances in modeling earth systems·2023
See all related articles

Related Experiment Video

Updated: Jun 6, 2025

Measurements of CO2 Fluxes at Non-Ideal Eddy Covariance Sites
09:05

Measurements of CO2 Fluxes at Non-Ideal Eddy Covariance Sites

Published on: June 24, 2019

7.9K

Tuning Earth System Models Without Integrating to Statistical Equilibrium.

Timothy DelSole1, Michael K Tippett2

  • 1Department of Atmospheric, Oceanic, and Earth Sciences George Mason University Fairfax VA USA.

Journal of Advances in Modeling Earth Systems
|November 29, 2024
PubMed
Summary
This summary is machine-generated.

This study introduces a new two-phase linear algorithm for estimating parameters in Earth System Models (ESMs), even with climate drift. This method improves accuracy for short simulations, offering a promising approach for climate model tuning.

Keywords:
autoregressive modelskalman filtermodel tuning

More Related Videos

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
13:27

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface

Published on: June 8, 2015

8.7K
Integrating Remote Sensing with Species Distribution Models; Mapping Tamarisk Invasions Using the Software for Assisted Habitat Modeling SAHM
12:26

Integrating Remote Sensing with Species Distribution Models; Mapping Tamarisk Invasions Using the Software for Assisted Habitat Modeling SAHM

Published on: October 11, 2016

13.3K

Related Experiment Videos

Last Updated: Jun 6, 2025

Measurements of CO2 Fluxes at Non-Ideal Eddy Covariance Sites
09:05

Measurements of CO2 Fluxes at Non-Ideal Eddy Covariance Sites

Published on: June 24, 2019

7.9K
Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
13:27

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface

Published on: June 8, 2015

8.7K
Integrating Remote Sensing with Species Distribution Models; Mapping Tamarisk Invasions Using the Software for Assisted Habitat Modeling SAHM
12:26

Integrating Remote Sensing with Species Distribution Models; Mapping Tamarisk Invasions Using the Software for Assisted Habitat Modeling SAHM

Published on: October 11, 2016

13.3K

Area of Science:

  • Climate Science
  • Computational Modeling
  • Statistical Analysis

Background:

  • Earth System Models (ESMs) are crucial for climate prediction but parameter estimation is challenging.
  • Simulations often exhibit climate drift before reaching statistical equilibrium, complicating parameter estimation.
  • Existing methods can yield unsatisfactory parameter estimates, particularly for short or drifting simulations.

Purpose of the Study:

  • To develop and evaluate a novel algorithm for robust parameter estimation in Earth System Models (ESMs).
  • To address limitations in current methods when dealing with non-equilibrium simulations and climate drift.
  • To improve the accuracy and reliability of parameter estimates for ESMs, specifically the Community Earth System Model version 2 (CESM2).

Main Methods:

  • The study proposes treating ESM time series as outputs of an autoregressive process.
  • A new strategy divides the parameter estimation into two linear phases to overcome nonlinear system limitations.
  • The algorithm is applied to estimate parameters within the convection scheme of the Community Earth System Model version 2 (CESM2).

Main Results:

  • The modified algorithm successfully produces accurate parameter estimates from perturbation runs as short as 2 years.
  • The method effectively handles simulations exhibiting climate drift, yielding comparable accuracy to methods that do not explicitly account for it.
  • Initial results demonstrate the autoregressive approach's potential for rigorous statistical framework-based model tuning.

Conclusions:

  • The proposed two-phase linear algorithm offers a promising strategy for tuning Earth System Models (ESMs) by explicitly accounting for climate drift.
  • Accurate parameter estimation is achievable even with short simulations and inherent climate drift.
  • Current performance limitations are likely technical and amenable to future investigation and improvement.