We have calculated linear temperature trends (in degree C per decade) in order to establish the influence of the unusually warm El Nino year of 1998. Our OLS coefficients for the surface (GHCN v2), radiosonde (NCEP Reanalysis), and MSU data (Channel 2 Lower Troposphere) are as follows:
'79-'95 | '79-'96 | '79-'97 | '79-'98 | '79-'99 | |
Surface | +0.080 | +0.109 | |||
Rad-sonde (500mb) | -0.017 | +0.033 | |||
MSU | -0.006 | -0.003 | +0.002 | +0.046 | +0.036 |
As can be seen, the MSU trends are close to zero before 1998. Its trend value for 1979-1999, with 1998 deleted, is -0.0003. In order to better understand the disparity between surface and atmospheric data, we investigated the latitude, altitude (for NCEP), and seasonal dependence of all the trends. We also calculated separate trend values for two periods, '79-'98 and '89-'99.
We conclude from this analysis that the surface trends are not credible. Further evidence comes from the fact that the well-controlled surface temperature data for the United States do not show an appreciable post-1940 warming, in contrast to the global surface data. In addition, proxy data from tree rings, ice cores, etc. show no post-1940 warming: Many even show a cooling trend after 1940.
1. National Research Council. "Reconciling Observations of Global Temperature Change." National Academy Press. Washington, DC. Jan, 2000.