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nao influences
In summer, a strong NAO- is thought to contribute to a weakened jet stream that normally pulls zonal systems into the Atlantic Basin contributing significantly to excessively long lasting heat waves over Europe. On inter‐annual timescales the significant part of the global climatic variation can be linked to ENSO (Webster et al., 1998). Derived from Hadley Centre Sea Ice and Sea Surface Temperature (HadISST) dataset, there are monthly IOD from 1870 to present, maintained by the Japan Agency for Marine‐Earth Science and Technology (JAMSTEC) (http://www.jamstec.go.jp/frsgc/research/d1/iod/iod/dipole_mode_index.html). cpc.ncep.noaa.gov/products/precip/CWlink/pna/nao.shtml, http://www.jamstec.go.jp/frsgc/research/d1/iod/iod/dipole_mode_index.html, http://www.esrl.noaa.gov/psd/data/correlation/pdo.data, Strengthen the influences of ENSO on the precipitation occurrence in the lower Yangtze River basin and weaken the influences of PDO on the precipitation occurrence in the southwestern part of Yangtze River basin, Weaken the influences of ENSO on both the precipitation occurrence and intensity in the lower Yangtze River basin, Weaken the influences of IOD on the precipitation occurrence in the centre part of Yangtze River basin, Weaken the influences of ENSO on the precipitation intensity in the lower and southwestern part of Yangtze River basin, Weaken the influences of ENSO on the precipitation intensity in the southwestern part of Yangtze River basin, Weaken the influences of IOD on the precipitation intensity in the west part of Yangtze River basin.
Spatiotemporal Precipitation Variability Modeling in the Blue Nile Basin: 1998–2016. Influence of Asian-Pacific Oscillation on Precipitation in Central Eastern China during Autumn (1960–2016).
(2009) that summer rainfall will be more than normal in South China (centred in Hunan province) in the years of positive IOD occurring independently. Integrating ecosystem services into effectiveness assessment of ecological restoration program in northern China's arid areas: Insights from the Beijing-Tianjin Sandstorm Source Region. For winter, the precipitation in the southwestern and southeastern parts of Yangtze River basin have been influenced by the positive ENSO event at the same year, however, the positive ENSO event at the same year tends to only increase the intensity of precipitation events in southwestern parts of Yangtze River basin while both the occurrence and intensity of precipitation events have been increased in southeastern parts of Yangtze River basin. They found that, even though NAO does not significantly affect the weather in the midwest, there was a significant increase in abundance of common grasshopper species (i.e. Spatiotemporal Variability of Extreme Summer Precipitation over the Yangtze River Basin and the Associations with Climate Patterns. Non‐stationarities in the occurrence rate of heavy precipitation across China and its relationship to climate teleconnection patterns. And these may be caused by an anomalous lower‐tropospheric anticyclone (cyclone) located in the western North Pacific during the ENSO event (Wang et al., 2000; Chen et al., 2013). [14], On the East Coast of the United States an NAO+ causes warmer temperatures and increased rainfall, and thus warmer, less saline surface water. Hydrological Processes in the Huaihe River Basin, China: Seasonal Variations, Causes and Implications. One of these patterns is the air pressure difference between the Arctic and mid-latitudes: the so-called Arctic oscillation with the Azores highs and Iceland lows known from the weather reports. Number of times cited according to CrossRef: Changes in consecutive dry/wet days and their relationships with local and remote climate drivers in the coastal area of China. Meanwhile, there are many articles analysing the summer monsoon in the Yangtze River basin and the associated large scale circulation, it has been well studied that the East Asian Monsoon has been significantly influenced by the ENSO (Chen et al., 2013). The NAO was disc (2012) found that it is the occurrence of rainfall events, rather than the average intensity of rainfall during the events that is the dominant mechanism driving seasonal rainfall changes caused by ENSO, IOD and the southern annular mode. Decreased Streamflow in the Yellow River Basin, China: Climate Change or Human‐Induced?. And the positive ENSO event a year earlier tends to increase the intensity of precipitation events in the east part of the Yangtze River basin, however, the positive ENSO event at the same year tends to decrease both the occurrence and intensity of precipitation events in the southeastern part of the Yangtze River basin. In summary, these will provide valuable information for improving the long‐term forecasting of precipitation based on the relationship with ENSO, NAO, IOD and PDO, and will be helpful for planning and development of agricultural activities under influences of the natural climate variability. In recent years, the possible influences of ENSO events on precipitation regimes in both space and time have been receiving increasing attention, and many researchers have found significant influences of ENSO events on precipitation events at different places, e.g. [22], In the north western part of the Atlantic, both of these winters were mild, especially 2009–2010, which was the warmest recorded in Canada.
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