By Stella Rimington
MI5 Intelligence Officer Liz Carlyle is summoned to a gathering together with her boss Charles Wetherby, head of the Service's Counter-Espionage department. His counterpart over at MI6 has obtained alarming intelligence from a high-placed Syrian resource. a center East peace convention is deliberate to occur at Gleneagles in Scotland and a number of other heads of country will attend. The Syrians have discovered that everyone is mounting an operation to disrupt the peace convention in a manner designed to be unbelievable, laying the blame at Syria's door.The resource claims that Syrian Intelligence will act opposed to the pair, possibly by way of killing them. not anyone understands who they're or what they're planning on doing. Are they operating jointly? who's controlling them? Or is the complete tale a delicately laid path of incorrect information? it's Liz's activity to determine. yet, as she discovers, the risk is much more than she or somebody else may have imagined. the way forward for the complete of the center East is at stake and the convention closing date is drawing ever nearer.
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Additional resources for Dead Line (Liz Carlyle, Book 4)
9) The graph of function ",(ex) is given in Fig. 10. The coefficient of variation of the flood component of mean discharge is given by (10) The value Qmin is the minimum of mean discharge for a certain interval, for example 30-days. The increase of k conditions the increase of the probability that this certain interval includes the part of one or several floods. The flood component of Qmin depends on k and the height, volume and duration of flood peaks. m,,) = E(Qrnin) - E(q o) =qqJ[k,m(v)] (11) 32 Equation (11) is an approximation arrived at with the help of a simulation experiment.
M. (\993) Hydro-Climatic Data Network (HCDN) : Streamflow Data Set, 1874-1988 . USGSWaterResources Investigations Report 93-4076 (CD-ROM) . M . A. su 1. Introduction The spatial structure of long-term fluctuations of river runoff has been studied for a long time in connection with research on the genesis of these fluctuations and attempts to establish their global and large-scale laws. One of the directions of this research is the identification of areas with synchronous and asynchronous fluctuations of annual runoff.
However, for some rivers the function 'Prit) linearly growing in the interval lt I , tk 1 was used. In this it case depends on the flood component of the runoff volume for the whole period. Number k is a characteristic of this volume and correlation between qo and k reflects this dependence. 46, and for the River Lornnitsa (Ukrainian Carpathians) corrtqs. 47. For functions rpft - tj) formulas of Goodrich or Sokolovsky, or Reits-Crepps can be used. In some cases the recession curve was described by a pair of exponents: one for the first 2 or 3 days and the other for the next .
Dead Line (Liz Carlyle, Book 4) by Stella Rimington