Power grid galloping long-term prediction method and system based on climatic dynamic downscaling
A prediction method and downscaling technology, applied in the field of long-term grid galloping prediction method and system based on climate dynamics downscaling, can solve problems such as inability to predict grid galloping in the long term, achieve safe and stable operation, simple calculation process, and good versatility Effect
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Embodiment 1
[0035] The long-term prediction method for power grid galloping based on climate dynamic downscaling in this embodiment includes the following steps:
[0036] S1. Select the global climate model, predict the monthly average meteorological field in the next N months, and output the meteorological data. The meteorological data output by this model meet the following conditions: it can provide the lateral boundary field and underlying surface field for the regional climate model in the next step, such as: the meteorological elements of the lateral boundary field and underlying surface field include sea surface temperature, soil temperature, Layer-by-layer geopotential height field, temperature field, wind field and specific humidity field at 1000hPa and above.
[0037] Since global climate models generally have low resolution, downscaling predictions from more refined regional climate models are required.
[0038] S2. Select a regional climate model (meteorological model), divid...
Embodiment 2
[0047] The present invention also provides a computer system, including a memory, a processor, and a computer program stored in the memory and operable on the processor. When the processor executes the computer program, the steps of any of the above-mentioned methods are realized.
[0048] In actual forecasting, since the global climate model cannot make refined predictions, and the meteorological model (regional climate model) suitable for carrying out refined predictions cannot be integrated for a long time due to the accumulation of errors, the present invention combines the advantages of the two to perform long-term predictions, and has the following advantages:
[0049] On the one hand, the lateral boundary field and underlying surface are provided by the global climate model, which ensures that the forcing items of the meteorological model are updated regularly;
[0050] On the other hand, meteorological models can simulate the area to be predicted at a higher spatial and...
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