气候变化领域集成服务门户

Gaps with missing data in the observational temperature record are responsible for an underestimation of the global warming between 1881-1910 and 1986-2015 by 0.1 degrees C. We found that missing data in the historical observations introduce a warm bias in the early part of the record and a cold bias toward the end. The effect of the nonuniform sampling was explored by comparing the global mean temperature estimated from gridded observations, climate model simulations, and reanalysis. Output from global simulations was subsampled by masking the grid boxes corresponding to those with missing data in the observations to mimic the geographical availability of temperature measurements. A combination of variance depending on region and a varying geographical data sampling over time explains the bias in the global mean. We propose a methodology for estimating the global mean temperature that reduces the effect of the nonuniform variance.