How has cyclone formation changed since the 1990s

Since the 1990s, several factors have contributed to changes in cyclone formation: 1. Global warming: Rising sea surface temperatures due to climate change provide more energy for cyclone formation and intensification. 2. Oceanic and atmospheric cycles: Natural climate variability, such as the El Niño-Southern Oscillation and Pacific Decadal Oscillation, can affect cyclone formation patterns. 3. Changes in wind patterns: Alterations in atmospheric circulation patterns can influence cyclone development and tracks. These changes result from various factors, including climate patterns and human-induced alterations. 4. Increased satellite observation: Advances in technology and satellite coverage have improved the detection and monitoring of cyclones, leading to higher reported numbers. 5. Data quality and consistency: Improved data collection practices and an increasing number of reporting stations have likely contributed to higher detection and documentation of cyclones. 6. Urbanization and deforestation: Changes in land use can alter the landscape and affect the local climate, potentially influencing cyclone formation in certain regions. It is important to note that while these factors contribute to changes in cyclone formation, it is challenging to attribute specific events solely to one factor. Cyclone formation is a complex process influenced by numerous variables.