3.1. DA in Chinese airports
The DA values across Chinese airports exhibit a clear geographical trend: lower DA values in Eastern China, intermediate DA values in Central China, and higher DA values in Western China (
Figure 1b). This pattern is intrinsically linked to the varying altitudes of these regions (
Figure 1a). The Eastern region, featuring coastal plains and hilly lands, is home to airports with lower altitudes. Consequently, most airports in this region report DA values ranging from 1000 to 3000 feet. This lower DA promotes more efficient aircraft performance, due to the denser air which provides greater lift and engine power. Moving inland, Central China's more diverse topography, characterized by basins and rolling plateaus, yields airports with moderately higher altitudes. Accordingly, the DA in these areas typically lies between 4000 and 9000 feet. These elevated DA values require pilots to adjust their flight operations, as they can lead to decreased engine power, lower climb rates, and longer take-off and landing distances. In Western China, the geographical landscape becomes even more dramatic, dominated by the towering heights of the Tibetan Plateau. Airports in these areas exist at substantial altitudes, causing the DA to exceed 9000 feet. This high DA imposes significant operational considerations, as the reduced air density can further diminish engine performance and increase take-off and landing distances. This trend underscores a close correlation between the DA and geographical elevation. Each regional characteristic, from the coastal plains of the East to the high plateaus of the West, contributes distinctively to the DA values, which in turn significantly influences airport and flight operations across China.
In the future timeframe of 2081-2100, we observe a noteworthy shift in the DA ranging from 200 to 800 feet across China, signifying substantial variations in aviation conditions. There is an east to west gradient in these changes, suggesting that the DA changes escalate notably as one moves from the eastern to the western regions of the country. In the eastern region of China, characterized primarily by its flat, low-altitude terrain, the DA tends to shift by approximately 200-400 feet. When considering the central part of the country, the landscape undergoes a noticeable transition. The terrain height increases, and it is therefore unsurprising to witness an accompanying rise in the DA changes to about 400-600 feet. Moving further to the Western region, the terrain is predominantly characterized by high-altitude plateaus. It is within these challenging terrains that the most significant DA changes take place, often exceeding 600 feet. The predicted DA changes are likely to have significant implications for flight operations across the country, and thus necessitates continual monitoring and adaptation by the aviation industry to ensure safety and efficiency in the face of these changing conditions.
Figure 2 provides a quantitative illustration of the number of airports expected to experience varying degrees of explicit DA changes. The largest subset of airports - a total of 95, accounting for 39.1% of all airports - are projected to confront DA increases of 500-600 feet. Moreover, a further 55 airports, which represent 22.6% of the total, are anticipated to face DA increases within the range of 400-500 feet. Additionally, a group of 45 airports, comprising 18.5% of all airports, are estimated to undergo DA fluctuations of 600-700 feet. Such a significant shift will almost certainly necessitate meaningful adaptations in flight operations, including alterations in payload, modifications to fuel efficiency strategies, and adjustments in take-off and landing distances. A smaller yet crucial group of 10 airports, accounting for 4.1% of all airports, are forecasted to experience substantial DA increases ranging between 700-800 feet. Despite their smaller quantity, these airports will likely be confronted with significant challenges, given the substantial magnitude of these projected DA alterations. Simultaneously, there are 38 airports, representing 15.6% of all airports, that are projected to encounter DA shifts in the comparatively lower range of 200-400 feet. Although these changes may seem less severe compared to others, they still demand meticulous consideration, foresight, and planning to ensure operational safety and efficiency.
3.2. The contribution of temperature to DA
Changes in DA are predominantly attributed to alterations in surface air temperature and surface pressure. To discern the distinct influences of these two factors, we conducted a detailed analysis, keeping the surface pressure values constant at 1995-2014 levels while applying projected temperature values for the periods of 2081-2100. This approach allows us to isolate and explicitly quantify the direct contribution of surface air temperature to DA changes.
Our research illustrates a noticeable trend that the ascension of temperatures is leading to a consistent rise in DA across all airports in China for the predicted period of 2081-2100 (
Figure 3a). This observed pattern is more discernible in the southern regions, demonstrating moderate yet significant escalations in central China, and culminating in remarkable elevations in the northern areas. In the case of southern China, the anticipated rise in DA as a consequence of temperature fluctuations is about 450 feet. In stark contrast, northern China may witness a more pronounced alteration in DA exceeding 550 feet. Of all regions, the northwest of Xinjiang province stands out as it is expected to endure the most considerable temperature-induced DA alterations, with increases potentially surpassing 800 feet.
These observed shifts in DA are found to correspond directly with changes in temperature (
Figure 3b). To elucidate, the progression of temperature alterations escalates from south to north, starting with a rise of approximately 3°C in southern China, around 5°C in the central regions, and surging to over 6°C in northern China. The apex of these temperature changes is discovered in the northwest of Xinjiang province. The distinctive climatic conditions of this region, characterized by its extreme climate and high-altitude environment, exacerbate the impact of temperature changes on DA. This particular situation underscores the pivotal role that surface air temperature plays in influencing DA. As we stand on the brink of a future where global temperatures continue to ascend, these findings accentuate the urgency for implementing climate-adaptive strategies in the aviation sector. This is crucial to maintaining optimal flight performance and ensuring safety, especially in light of the increasing demands and challenges posed by climate change.
In order to provide a comprehensive numerical representation of the number of airports, we conducted a statistical analysis in
Figure 4. As depicted in the diagram, the effect of projected temperature changes primarily influences an increase in the DA range from 300 to 800 feet. It is noteworthy to highlight that the majority of airports experience a DA alteration within the range of 500-600 feet. This category accounts for a substantial 42.8% of all surveyed airports. Further analysis of the data reveals that there are 70 airports that have registered DA changes within the 600-700 feet range, attributable to the aforementioned projected temperature variations. These constitute a significant 28.8% of all examined airports. Moreover, an additional 55 airports, representing 22.6% of the total, are reported to have DA shifts within the same range of 600-700 feet. However, the extremes of the DA change spectrum, specifically the 300-400 feet and 700-800 feet ranges, are found to be less impacted by temperature fluctuations. Thus, the number of airports reporting DA changes within these intervals due to projected temperature changes remains relatively low. This data suggests that the temperature impacts on airport DA change are not uniformly distributed but exhibit a certain trend favoring a particular range.
3.3. The contribution of surface air pressure to DA
In addition to the temperature's influence on DA, we further investigated the impact of surface pressure changes on DA variations. To do this, we held temperature levels constant to those in 1995-2014, then recalculated DA using projected surface air pressure values for the periods 2081-2100. We then evaluated the differences between these recalculated DAs and the original DAs from 1995-2014, thus isolating the effect of surface pressure changes.
Our comprehensive analysis elucidates that alterations in surface pressure wield a unique and significant influence on Density Altitude (DA), the extent of which varies geographically, as illustrated in
Figure 5a. In the eastern part of China, particularly north of the Yangtze River, the majority of airports are predicted to confront an escalation in DA as a consequence of changes in surface pressure. However, the degree of these increases remains relatively minimal. This is primarily attributable to a slight decrease in pressure within this region, as demonstrated in
Figure 5b. Conversely, a substantial number of airports situated in regions beyond the east are expected to witness a coherent decline in DA. This involves changes approximating -50 feet in the central areas and plunging below -100 feet in most of the western regions. This phenomenon can be traced back to an anticipated rise in pressure during the 2081-2100 periods within these geographical locations. An area of particular interest lies in the southern and western peripheries of the Qinghai-Tibet Plateau, where the surface pressure changes tend to have an extraordinarily pronounced effect on the DA. A decrease in surface pressure in these regions results in a dramatic reduction of DA, with projected reductions surpassing 200 feet.
In an effort to quantify the number of airports for each range of explicit DA alterations, we have conducted a comprehensive statistical analysis, the results of which are depicted in
Figure 6. As demonstrated in the said Figure, the implications of projected changes in surface air pressure on DA values present a more intricate scenario compared to the effects induced by temperature changes. Here, the majority of the airports are observed to experience a reduction in DA, while a minority of them show a tendency towards increased DA. Our data reveal that there are 152 airports that display DA changes within the range of -100 to 0 feet, which can be attributed to the predicted alterations in surface air pressure. This subset represents a significant 62.6% of all surveyed airports. Furthermore, 25 airports, amounting to 10.3% of the total number, show DA shifts ranging from -200 to -100 feet due to similar changes in surface air pressure. In comparison, the number of airports experiencing DA changes within the range of 0 to 100 feet due to projected surface air pressure changes appears to be relatively minimal.
While the effects of temperature changes on DA are broad and generally increasing, surface pressure changes can lead to both increases and decreases in DA, depending on the geographical region. This illustrates the complexity of DA changes and the need for region-specific adaptive strategies in aviation. What seems apparent from these findings is that, in most airports, the anticipated changes in surface air pressure are likely to counterbalance the impact of temperature changes on DA. This suggests a nuanced interplay between different atmospheric variables in influencing DA, making it crucial for future climate models and aviation planning to consider these combined effects.
From our analysis, it's evident that compared to the impacts of projected surface air temperature variations on DA, the influence of projected surface pressure changes on DA is relatively less pronounced. This analysis holds true even though the projected variations for both temperature and pressure appear to be of similar magnitudes. The reason behind this phenomenon can be attributed to the manner in which DA responds to changes in temperature and surface pressure. Specifically, DA varies in direct proportion to the changes in temperature and surface pressure with respect to their respective base values. That is, a unit change in temperature or surface pressure from their base values will result in a proportional change in DA. However, it's critical to note that the base values of surface air pressure are significantly larger than those of surface air temperature. As a result, even though temperature and pressure changes might be similar in magnitude, the relative changes in temperature from its base values tend to be more significant than those of surface pressure from its larger base values. This results in temperature variations having a more pronounced effect on DA changes compared to surface pressure variations. Therefore, it's crucial that this differential sensitivity of DA to temperature and pressure changes be considered in the modeling of future climate scenarios and the development of responsive strategies in aviation planning.