scholarly journals 中国东部冬季气温与海平面气压异常的关系Analyses of the Winter Air Temperature in Eastern China and the Sea-Level Pressure Anomaly

2012 ◽  
Vol 02 (02) ◽  
pp. 68-73
Author(s):  
陈 少勇
2011 ◽  
Vol 108 (1-2) ◽  
pp. 173-189 ◽  
Author(s):  
C. D. Papadimas ◽  
A. Bartzokas ◽  
C. J. Lolis ◽  
N. Hatzianastassiou

2012 ◽  
Vol 25 (16) ◽  
pp. 5600-5611 ◽  
Author(s):  
Fengying Wei ◽  
Lei Hu ◽  
Guanjun Chen ◽  
Qian Li ◽  
Yu Xie

Abstract A close relationship between sea level pressure (SLP) over East Asia and precipitation indices (PIs) in eastern China was observed in the summers (June–August) of 1850–2008 using singular value decomposition (SVD) analysis. To investigate this relationship over a longer period, the SLP fields were reconstructed back to 1470 based on a mathematical model and the historical precipitation indices of eastern China. A cross-validation test of independent samples suggests that the reconstructed SLPs are statistically acceptable. According to the first three predominant SVD modes of the SLP field, three SLP index series (SLPI1–SLPI3) were developed to quantify the thermodynamic differences among the critical SLP centers of East Asia. Both SLPI1 and SLPI2 are highly correlated with the East Asian summer monsoon index, whereas SLPI3 is related to the index of Eurasian meridional atmospheric circulation. The temporal scales of SLP indices were examined during 1470–2008 using the wavelet power spectra. Results indicate that there is significant variance at a 2–5-yr band in the power spectra of the three SLP indices, suggesting SLPI1–SLPI3 have evident interannual variability. Moreover, the wavelet power spectra of SLPI1 and SLPI2 show significantly higher power at the 8–12-yr scale from 1470 to 1750 and at the 60–90-yr scale after 1750. For SLPI3, besides the interannual variability, it has additional periodical variability of 6–11 and 23–33 yr.


2016 ◽  
Vol 49 (4) ◽  
pp. 1321-1339 ◽  
Author(s):  
Ruiqiang Ding ◽  
Jianping Li ◽  
Yu-heng Tseng ◽  
Cheng Sun ◽  
Fei Zheng

2011 ◽  
Vol 139 (5) ◽  
pp. 1569-1582 ◽  
Author(s):  
David Werth ◽  
Alfred Garrett

One year’s worth of Global Forecast System (GFS) predictions of surface meteorological variables (wind speed, air temperature, dewpoint temperature, sea level pressure) are validated for land-based stations over the entire planet for forecasts extending from 0 h into the future (an analysis) to 7 days. Approximately 12 000 surface stations worldwide were included in this analysis. Root-mean-square errors (RMSEs) increased as the forecast period increased from 0 to 36 h, but the initial RMSEs were almost as large as the 36-h forecast RMSEs for all variables. Typical RMSEs were 3°C for air temperature, 2–3 mb for sea level pressure, 3.5°C for dewpoint temperature, and 2.5 m s−1 for wind speed. An analysis of the biases at each station shows that the biggest errors are associated with mountain ranges and other areas of steep topography, with land–sea contrasts also playing a role. When the error is decomposed into the bias, variance, and correlation terms, the large initial RMSEs for the 0-h forecasts are seen to be due to a large forecast bias (which persisted into the longer forecasts) with errors in forecast correlation also making a large contribution. A validation of two subdomains showed results similar to the global validation, but the dependence of the biases on the forecast time was clearer. Finally, the RMSE values climb as forecasts go out when validated out to a period of 7 days as the correlation error term grows.


Author(s):  
R. T. Omond

The barometer at the Fort-William Observatory is 42 feet above sea-level, and its readings are reduced to sea-level by the ordinary tables based on Laplace's formula; but in reducing the barometer at the Ben Nevis Observatory, which is 4407 feet above sea-level, use is made of a table specially constructed by Dr Buchan, and described by him in the first volume of the Ben Nevis Observations (see Transactions, vol. xxxiv. p. 24). This table consists of the average values of the difference between the barometer on Ben Nevis and that at sea-level in Fort-William, for each successive tenth of an inch of sea-level pressure and each degree of air temperature.


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