I have used is a very simple alternative method for calibrating the temperature of the sample compared to that of the variable temperature unit. This is illustrated in the figure below.
A "sample" is prepared by pushing a NONMAGNETIC thermocouple through an NMR tube cap. The depth of the thermocouple is adjusted such that when the cap is put on the NMR tube, the tip of the thermocouple sits in the center of the rf coil. The NMR tube should contain a suitable liquid filled to the correct depth. The tube is placed in the spinner and set to the proper depth with a depth gauge. While holding onto the thermocouple, the sample is lowered into the magnet until it sits correctly in the NMR probe. The thermocouple is connected to a digital thermometer (some of these devices can use a second thermocouple in an ice water bath as a reference). The desired temperature is set on the variable temperature unit. When the temperature on both the variable temperature unit and digital thermometer have stabilized (~ 10 minutes), the values from each are recorded. This is repeated for temperatures over the desired temperature range and a calibration plot is constructed. Shimming is not an issue. Note that no NMR measurements are made and that the sample tube is not spinning.
A "sample" is prepared by pushing a NONMAGNETIC thermocouple through an NMR tube cap. The depth of the thermocouple is adjusted such that when the cap is put on the NMR tube, the tip of the thermocouple sits in the center of the rf coil. The NMR tube should contain a suitable liquid filled to the correct depth. The tube is placed in the spinner and set to the proper depth with a depth gauge. While holding onto the thermocouple, the sample is lowered into the magnet until it sits correctly in the NMR probe. The thermocouple is connected to a digital thermometer (some of these devices can use a second thermocouple in an ice water bath as a reference). The desired temperature is set on the variable temperature unit. When the temperature on both the variable temperature unit and digital thermometer have stabilized (~ 10 minutes), the values from each are recorded. This is repeated for temperatures over the desired temperature range and a calibration plot is constructed. Shimming is not an issue. Note that no NMR measurements are made and that the sample tube is not spinning.
The energy levels are no longer equally spaced. Furthermore, the position of the resonances resulting from the transitions depends on the orientation of the nucleus with respect to the magnetic field. Since all orientations are represented equally in a powder sample, each transition gives a
The spectrum consists of a central transition, CT, and two satellite transitions, ST1 and ST2. Note that along with a lineshape due to the orientational dependence of the nucleus in the magnetic field, there is also an isotropic quadrupolar shift. The central and satallite transitions are not at the same frequency. This effect is completely separate from the chemical shift.

The cross-peaks highlighted in yellow in the top panel of the figure are expanded in the bottom panel. Black contours are positive and red contours are negative. The panel on the bottom left shows the cross-peaks for AX and BX. In the case of the AX cross-peak, the line drawn through the cross peak has a positive slope indicating that the passive couplings JAB and JBX are of opposite sign. The line drawn through the BX cross peak also has a positive slope indicating that the passive couplings JAB and JAX are of opposite sign. From this we can deduce that JAX and JBX are of the same sign. The panel on the bottom right shows the cross-peak for AB. In this case, the line drawn through the cross peak has a negative slope confirming that the passive couplings JAX and JBX are of the same sign. In conclusion, the geminal and vicinal coupling constants are of opposite sign.