Gratuitous 发表于 2025-3-28 16:55:06
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http://reply.papertrans.cn/79/7809/780805/780805_42.pngforecast 发表于 2025-3-29 02:42:27
Alfred Benninghoven,Lothar Wiedmannnal and theoretical limitations the actual damping rate is uncertain even now; a decay time of 45–70 years or more seems probable. The two most likely candidates for dissipating wobble energy are mantle anelasticity and a dynamic response of the oceans to wobble. Because of the frequency dependence善于骗人 发表于 2025-3-29 06:25:04
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http://reply.papertrans.cn/79/7809/780805/780805_45.pngfleeting 发表于 2025-3-29 14:37:01
Alfred Benninghoven,Lothar WiedmannSpatially, the ocean varies with water depth, ocean currents, and oceanic fronts. This abiotic and biotic variability makes managing resources in the dynamic ocean environment extremely difficult, and as a result, fisheries management often serves as one of the textbook examples of an unstructured o