Page 35 - ITU Journal Future and evolving technologies Volume 2 (2021), Issue 7 – Terahertz communications
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ITU Journal on Future and Evolving Technologies, Volume 2 (2021), Issue 7































          Fig. 1 – Bit error rate versus SNR “waterfall” plots for an M‑QAM communication system, with M = 2, 4, 16, 64, and 256. Higher‑order modulations
          have closer symbol spacing under equivalent power requirements, resulting in a higher SNR required for equivalent error performance to a lower order
          modulation, assuming the absence of group velocity dispersion.

          2.  METHODOLOGY                                      gether these terms determine the complex index of refrac‑
                                                               tion of the atmosphere. This complex index is obtained by
          In  order  to  quantitatively  measure  the  impact  of  ISI
                                                               a combination of Molecular Response Theory (MRT) [23]
          caused  by  atmospheric  GVD,  bit  error  rate  simulations   and continuum effects [24, 25], in which the broadened
         were performed using a channel model founded upon an   absorption  lines  of  all  the  H O  and  O molecular  reso‑
                                                                                        2
                                                                                                 2
          accurate  understanding  of  atmospheric  molecular  reso‑   nances from 0 to 5 THz are found by MRT , summed, then
          nances.  It  is  from  this  atmospheric  model  that  all  the   added to the continuum absorption. This has been shown
          effects accounted for in this work were derived.  Speci i‑   to accurately model atmospheric behavior over the sub‑
          cally,  the  channel  considered  in  this  study  was  a  Linear   terahertz bands, and accounts for the contribution of all
         Time‑Invariant  (LTI)  channel  with  Additive  White  Gaus‑   relevant molecular resonances up to 5 THz.
         sian  Noise  (AWGN)  and  no  obstruction,  multipath  pro-
         pagation,  or  Doppler  effects.  However,  the  transfer   In addition to the atmospheric effects,  pulse shaping  il‑
         function of the atmosphere itself was modeled as variable   ters also shape the transmitted waveform, limit the band‑
         over frequency  in  both  absorption  and  refractive index,   width  of  the  signal,  and  reduce  ISI.  In  our  simulations,
         which gives rise to the behavior observed in our results.   a raised cosine  ilter    (  ) with a roll‑off factor of 1 was
                                                                                       
         Even though our assumption of an L TI AWGN channel is   used,  and  incorporated  into  the  channel  model  by
         much  simpler    than   the   environments   usually   applying  it  directly  to  the  atmospheric  transfer  function
         encountered  by  wireless  link  designers  at  terahertz   in frequency domain, yielding a channel transfer function
         frequencies,  the  fact  that  our  results  arise  from  the      (  )  =     (  ) ×    (  ).  The impulse response of the
                                                                             
                                                                   
                                                                                    
         properties  of  the  atmosphere  rather  than  complex  and   complex channel transfer function can then be derived as
                                                                         −1
           ic  channel  effects  make  them  applicable        ℎ (  )  =  ℱ [   (  )],  where  ℱ −1   indicates  the  inverse
                                                                                
                                                                   
         to a wide range of channels, including those signi icantly   Fourier transform.
         more complex that that presented here [22].
                                                               Once  the  impulse  response  of  the  channel  is  known,  a
         The  atmospheric  transfer  function  is  described  most   data  vector  containing  complex  valued  communication
          generally  as     (  )  =    (  ) exp[−    (  )],  where    (  )   symbols  is  generated.  The  symbols  in  the  data  stream
                         
          and    (  )  are  the  frequency‑dependent  attenuation  and  occur with equal distribution, but the data stream is not
          phase shift imparted by the atmosphere, respectively,  completely  random.  Rather,  it  is  generated  such  that
                  √
          and    =  −1. This non‑unity transfer function arises  combinations  of  symbols  are  also  equally  distributed,  so
          from the interaction of various atmospheric gas species  every possible permutation of    symbols occurs an equal
         with terahertz‑frequency radiation. Most notable among  number  of  times  for  a  speci ied    .    This  is  necessary
          these are water vapor and diatomic oxygen, which exhibit  because   the   severity   of   ISI   experienced   by   a
          strong rotational and vibrational resonances within and  communication symbol  depends  on  the  value  and  order
          above the terahertz bands. While the amplitude (absorp‑  of  the  neighboring  symbols,  not  on  the  value  of  the
          tion) term of    (  ) is most often discussed, the phase  symbol  itself.  This  data  stream  is  convolved  with  the
                         
          term   (  ) is equally important to propagation, and to‑  channel  impulse  response,  resulting  in  a  sequence  of




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