We demonstrate that dispersive compensation can be achieved for the communication channels within the atmospheric THz windows using the long-path THz-TDS system. However, the THz pulse broadening cannot be eliminated due to the bandwidth reduction of the propagating THz pulse due to the frequency dependent absorption of the channels.There are many applications for relatively short-length, high bit-rate THz links in the atmosphere [1][2][3][4][5]. A recent study presented an experimental and theoretical characterization of short-length, high bit-rate links for the seven THz communication channels in the atmosphere below 1 THz [4]. Here, using the complete theoretical approach for the absorption and dispersion of water vapor [4-6], we show the potential to increase the bit-rate distance product, by dispersion compensation. However, we also show that the frequency dependent absorption within the channel significantly reduces the bandwidth of the transmitted signal. This reduction also broadens the THz data pulses, and consequently dispersion compensation cannot eliminate all of the observed pulse broadening with propagation. THz pulses experience distortion and broadening when they propagate through the dispersive atmosphere, which leads to overlapping of adjacent pulses in the bit sequence. Here, we analyze the increase of the performance of the Channel 7 at 852 GHz, with dispersion-compensation to demonstrate achievable high data rates of the future THz wireless network.Dispersion management compensates phase dispersion in communication channels. Such compensation has been studied since 1980, and is used in optical fibers to significantly increase the data rates in optical communications. It is also important to understand the full capacity of the THz channels without being limited by dispersion and to be able to estimate the dispersion tolerance of the THz channels.When the electric field of the input THz pulse, E(0,ω), (expressed as a function of frequency) passes through the dispersive atmosphere, the phase changes due to the resonance lines of water vapor. The output complex spectrum E (z,ω), is given by the product of the input field with the phase function and the attenuation, as