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Technical Note: Bias Adjusting Climate Model Projections

3 minutes read
Jan 31 2018
Technical Note: Bias Adjusting Climate Model Projections

We released our first technical note called "Bias Adjusting Climate Model Projections". This document provides an overview of our methods used to generate our ready-to-use climate projections and is intended for users who wish to learn more on the techniques used to process climate model data in climate change impact studies, from local to global scale. You can download the document on our page on researchgate.com: researchgate.net/publication/322888233_Bias_Adjusting_Climate_Model_Projections.

Bias adjustment, also known as bias correction, is a method used in climate science to correct systematic errors (biases) in climate model outputs. Climate models are sophisticated tools that simulate the Earth's climate system, but they can have discrepancies when compared to observed historical climate data. These discrepancies or biases can arise due to model imperfections, including assumptions made in the model, the spatial resolution of the model, or limitations in representing complex natural processes.

Here are some key aspects of bias adjustment in climate models:

  1. Purpose of Bias Adjustment: The primary goal is to align model outputs more closely with observed historical climate data. This process improves the reliability and accuracy of climate projections and is particularly important when models are used for impact assessments and decision-making in climate adaptation and mitigation.
  2. Correction of Systematic Errors: Bias adjustment involves statistical techniques that correct systematic errors in variables such as temperature, precipitation, wind speed, and humidity. The correction is typically done by adjusting the distribution of model outputs to match the distribution of observed data over a historical reference period.
  3. Methods: Various statistical methods are used for bias adjustment, including linear scaling, quantile mapping, variance scaling, and distribution-based approaches. The choice of method depends on the specific variable being corrected and the nature of the bias.
  4. Temporal and Spatial Considerations: Bias adjustment can be applied to different temporal scales (daily, monthly, seasonal, or annual) and spatial scales (local, regional, or global). The process takes into account the time and location-specific characteristics of climate data.
  5. Limitations and Challenges: While bias adjustment is a useful tool for improving model outputs, it has limitations. It assumes that the biases are consistent over time, which may not always be the case, especially under changing climate conditions. It also does not correct biases arising from missing or misrepresented physical processes in the models. Therefore, bias adjustment is often used in conjunction with other methods to improve model accuracy.
  6. Application in Climate Impact Studies: Bias-adjusted climate model outputs are widely used in climate impact studies, including hydrological modeling, agricultural impact assessments, and infrastructure planning. They help ensure that the projections used in these studies are more realistic and tailored to observed climate conditions.

Bias adjustment is a critical step in the climate modeling process, enhancing the applicability of model projections for practical decision-making and planning. It is an area of ongoing research, with scientists continuously developing and refining methods to more accurately represent the real world in climate models.

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