In this paper, we investigate a novel technique that reconstructs the observed time series and incorporates driving forces. Furthermore, to illustrate and test the technique, we consider a couple of predictive experiments using ideal time series provided by the logistic and Lorenz systems with specific driving forces. The preliminary results show this approach can improve prediction proficiency to some extent, and the external forces play a similar role to that of state variables. Short-term prediction is one of the difficult issues in climate change studies. Because of the complexity of short-term climate processes and lack of general knowledge underpinning its mechanisms, proficiency in prediction remains at a stand-still [1,2]. As for climate change in the 21st century, global warming is the most important factor, with many studies devoted to the topic. The possible causes range from change in natural forces (such as solar activity and volcanic emission) to human activities (such as green-house gases, sulfate emission in aerosols, and land use). In addition, the internal variability of climate systems should not be ignored either. However, no matter the cause of climate change, global warming in fact gives notice that climate processes are non-stationary. So far many climate predictive theories formulated in statistics and in nonlinear science are based on the hypothesis that the process is stationary, thus ergodicity theory can be used under such conditions to reconstruct the dynamics from an observed time series and establish predictive equations constructed from it.This reconstruction is at variance with the basic behavior of climate process. As is well-known for any weather or climate system, it is impossible to state the initial conditions incontrovertible. In fact, except for global warming, recent work has addressed the proper characterization of non-stationarity using weather and climate data. For instance, Tsonis [3] analyzed low-frequency (decadal to multi-decadal) variation in global precipitation over the past century and found that fluctuations about the global mean have increased significantly, implying that the second-order moment of the precipitation has changed on those scales, or that global precipitation process is non-stationary in the past century. In another case, Trenberth [4] found that the observed winter Pacific mean sea-level pressure underwent an abrupt change towards the end of the 70s; such a change in regime highlights the decline in the stationary behavior of the system. They noted that the behavior of these quantities is non-stationary. Most real world time series have some degree of non-stationarity due to external perturbations of the observed system [5].However, there is as yet no general theory about nonstationary processes. What scientists can do for the moment