Dynamic controls of the interannual and interdecadal variations of the freezing level height over the Tibetan Plateau

The variation of freezing level height (FLH) is significantly indicated the cryosphere change under global warming. In this study, the FLH during boreal summer in the TP regions is investigated, with the leading mode of a mono-sign pattern both on interannual and interdecadal timescales. The interannual variation of the summer FLH is dominantly coupled with the summer Arctic Oscillation (AO). When the AO is in positive phase, positive geopotential height anomalies are prolonged in the mid-latitude and negative anomalies are present over the Arctic regions. Meanwhile, the westerly shifts northward, preventing the cold air propagating southward. These conditions are beneficial for the surface and free-air temperature increasing and thus enhance the FLH over the TP. On the interdecadal timescale, the Pacific Decadal Oscillation (PDO) has mainly contributed to the variation of summer FLH. In the negative PDO phase, the warm sea surface temperature anomalies appear in the North Pacific, which could drive wave trains propagating eastward and induce high pressure in the TP. With the anomalous anticyclone from TP to western North Pacific, the easterly is prevalent in the TP. Consequently, the TP becomes warming remarkably and leads to the rising of FLH. This study provides an insight perspective for understanding the warming of TP, which also suggests the influence on the cryosphere processes at multi-timescale variations.