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Global Climate Change and Its Impacts


                   (1) Time Series Analysis Methods
                   Time series analysis stands as a widely applied and highly effective scientific method-
               ology, whose core lies in conducting in-depth exploration and analysis of chronologically
               ordered climate data to accurately reveal the long-term trends and cumulative characteristics
               inherent in climate change. In practical research implementation, the primary task involves
               collecting various climate data spanning sufficient temporal duration, encompassing cru-
               cial climate elements such as temperature, precipitation, sea level height, and atmospheric
               component concentrations. Taking the collection and analysis of global average temperature
               data as an example, researchers painstakingly undertake extensivegathering data spanning
               fromthe onset of the Industrial Revolution, covering temperature observation records from
               meteorological stations worldwide over a century or even longer periods. These datasets
               serve as keys that unlock insights into the long-term trends of climate change.
                   After obtaining the data, applying trend analysis methods from time series analysis be-
               comes a crucial step in identifying the overall direction of temperature changes over time.
               Among various trend analysis approaches, linear regression stands out as a commonly used
               and fundamental method. Its principle lies inconstructing a linear mathematical modelbe-
               tween temperatureand time, employing mathematical calculations to precisely quantify the
               averageannual temperature increase or decrease. Suppose linear regression analysis on global
               average temperature data from the past 100 years reveals a warming trend of 0.15°C per de-
               cade. This precise quantitative value acts like a lighthouse in the vast sea of climate change,
               clearly demonstrating the long-term cumulative effect of climate change on temperature over
               extended periods. It transforms from a vague concept into concrete numerical evidence that
               allows us to tangibly perceive Earth’s ongoing warming process.
                   In addition to trend analysis, seasonal decomposition in time series analysis also holds
               significant value. This method adeptly separates the seasonal components from the overall
               climate data, thereby revealing the variation patterns of climatic variables across different
               seasons within a year and the evolutionary trends of these patterns over long-term temporal
               scales. Taking precipitation data analysis as an example, by applying seasonal decomposition
               methods, researchers have clearly observed significant alterations in precipitation patterns in
               certain regions over the past few decades. This is specifically manifested in a gradual decline
               in summer precipitation and a slight increase in winter precipitation. Such long-term changes
               in inter-seasonal precipitation distribution are by no means coincidental; rather, they vividly
               exemplify the long-term cumulative effects of climate change in the realm of precipitation.
               This profoundly reflects the persistent impact of climate change on Earth’s hydrological cy-
               cle, subsequently triggering chain reactions across regional water resource distribution, agri-
               cultural production, ecosystem equilibrium, and numerous other aspects.
                   In the practical application of time series analysis, full consideration must be given to
               data noise and outlier issues. Climate data inevitably becomes subject to various interference
               factors during collection, transmission, and processing, resulting in noise and outliers. These



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