We investigate the time-of-night variation of solar neutrino rate which will be of relevance to SuperKamioka and Sudbury neutrino detectors in the framework of oscillations among the three flavors. An analytical method of computing the regeneration in the earth is presented. If day-night effect is seen, we show how the study of the time-of-night variation will allow the determination of the neutrino parameters.PACS number: 14.60. Pq, 95.30.Cq, 96.40.Tv, 96.60.Jw It has been known for quite some time that an asymmetry between night rate and day rate for the real time solar neutrino detectors is an unambiguous signal for neutrino mixing and oscillations. Conversely the absence of such an effect can put constraints on the neutrino masses and mixing angles. Although no day-night asymmetry outside the error-bars was seen at the Kamioka detector [1,2] the high statistics detectors like Super-Kamioka [3], SNO [4]and Borexino [5] will be much more effective in investigating this effect. If there is a day-night asymmetry, then the profile of the asymmetry as a function of the time during night is a very sensitive function of the neutrino parameters. The counting rates in these detectors are expected to be high enough for the study of this time-of-night variation. The aim of this note is to focus attention on this aspect of the day-night effect [6], in view of the fact that Super-Kamioka has already started functioning and SNO is expected to do so soon.The neutrino samples different amounts of matter in the earth during a single night and also during a year. The distance d travelled by the neutrino inside the earth during night, as a function of time t, is given byR is the radius of the earth, φ l is the latitude of the location of the detector, T D is the length of the day, T Y is the length of the year and zero of t is chosen at midnight on autumnal equinox. Thus assuming that the neutrino parameters are in a suitable range, neutrino data collected as a function of t contain an enormous amount of information on neutrino oscillations, which in principle can be analyzed to yield the neutrino parameters.The time variation of x = ( d 2R ) during the night and year are illustrated in Fig.1a. If the data collected during successive nights are accumulated at the corresponding x-bins, the calculation of neutrino rates per unit bin will require the function f (x) defined as the time duration per unit interval of x [7]. f (x) for different locations are plotted in Fig.1b, which shows the relative merits of the detectors for exposure to regions of x. We now describe an analytical method of calculating the neutrino regeneration effect in the earth. Let a neutrino of flavor α be produced at time t = t 0 in the core of the sun. Its state vector iswhere |νare the mass eigenstates with mass eigenvalues µ C i and U C αi are the elements of the mixing matrix in the core of the sun. We use Greek index α to denote the flavors e, µ,τ and Latin index i to denote the mass eigenstates i = 1,2,3. The neutrino propagates in the sun adiabatica...