A New Perspective on Increasing Activity of Extratropical Disturbances: Spatial and Temporal Trends of Wave Activity
Abstract
Changes in extratropical disturbance behavior could play an important role in climate dynamics and be responsible for a part of climate-related damage. However, robust observational evidence for long-term trends in the activity is still lacking, and understanding of how it is linked with climate phenomena is limited. In this study, we define an accumulated perturbation index (API) to quantify the variation in some scalar quantities of atmospheric disturbances. API measures the areas (e.g., % of total surface area of Earth) where a certain perturbation quantity exceeds the long-term mean value plus 0.5 standard deviations. This index reflects more realistically the ensemble impacts of a climate perturbation and/or trend (such as global warming and ENSO) on the extratropical disturbances, even though its impact on different regions might vary from year to year due to stochastic processes. API represents an integrated activity of extratropical disturbances at a given time relative to a long time span. API is calculated for the 5-day running mean and 10-30-day stream function fluctuations during DJF and JJA. The analysis reveals an increasing trend in API and variance of stream function, especially in the Southern Hemisphere. The findings suggest that atmospheric extratropical disturbances have strengthened in widening areas during the past six decades, even though there might not be robust trends in wave activity at regional scales. Whether the observed trends in API are associated with certain climate patterns is under investigation. Impact of global warming is likely one of the major sources for the increasing activity. The future change in API under global warming scenarios will be further studied by analyzing the projection of the CMIP5 models.
- Publication:
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AGU Fall Meeting Abstracts
- Pub Date:
- December 2016
- Bibcode:
- 2016AGUFM.A23H0323H
- Keywords:
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- 3305 Climate change and variability;
- ATMOSPHERIC PROCESSESDE: 3337 Global climate models;
- ATMOSPHERIC PROCESSESDE: 3339 Ocean/atmosphere interactions;
- ATMOSPHERIC PROCESSESDE: 3362 Stratosphere/troposphere interactions;
- ATMOSPHERIC PROCESSES