Seasonal variations in the temperatures of the hemispheres induce seasonal energy cycles between the hemispheres that drive tropical cyclones. Because the northern hemisphere has warmed more than the southern hemisphere, climate energy cycles develop between the hemispheres as well. The seasonal and climate energy cycles appear to interact among themselves, and tropical cyclone counts are affected by these interactions. Furthermore, the total number of tropical cyclones appears to have an increasing trend. The annual energy of tropical cyclones is nearly 1.46 × 10²² J yr⁻¹, and climate cycle energy is between 4.0 and 6.6 × 10²¹ J per cycle. The magnitude of the climate energy cycles is thus large enough to alter the energy and frequency of the tropical cyclones. Given that the climate is changing, the energy and frequency of tropical cyclones may be changing as well. The subject is broad and this work is limited to parameterization of the physics of energy oscillations between the hemispheres, demonstrating the existence of climate energy cycles, and revealing interactions between climate and seasonal energy cycles. Also, this parameterization may assist researchers in obtaining more and coordinated data relative to these cycles.

半球温度的季节性变化引起半球之间的季节性能量循环，从而驱动热带气旋。由于北半球比南半球变暖更多，气候能量循环也在半球之间发展。季节性和气候能量循环似乎相互影响，热带气旋数量也受到这些相互作用的影响。此外，热带气旋的总数似乎有增加的趋势。热带气旋年能量接近1.46×10 ²²  J yr ^-1，气候循环能量每个周期在4.0至6.6×10 ²¹  J之间。因此，气候能量循环的幅度足以改变热带气旋的能量和频率。鉴于气候正在变化，热带气旋的能量和频率也可能发生变化。该主题很广泛，这项工作仅限于半球之间能量振荡物理学的参数化，证明气候能量循环的存在，并揭示气候和季节性能量循环之间的相互作用。此外，这种参数化可以帮助研究人员获得更多与这些周期相关的协调数据。