#### Pulse resolution volume

Figure 1: The resolution cell

## What is the radar resolution?

#### Pulse resolution volume

The pulse resolution volume and resolution cell
characterizes the joint resolving capability according to the
range and
angular coordinates.
Usually, the pulse resolution volume is assumed to be limited by the
half-power beam width φ
of the antenna directivity pattern (−3 dB)
and the length Δt = τ_{i}/ 2,
with τ_{i} as the duration of the transmit pulse (or, in the case of
intra-pulse modulation,
by the duration of the signal at the output of the pulse compression device).

Figure 1: The pulse resolution volume or resolution cell

In the case of a very narrow
pencil beam,
i.e. with small values of the angles Θ_{az} and Θ_{el},
the size of the pulse resolution volume can be calculated according to the following equation:

V = R^{2}· |
c_{0}·τ |
· θ_{az} θ_{el} |
(1) |

2 |

The pulse resolution volume can also be considered as cylindrical depending on the used model of an approximation of the antenna pattern to simple geometric shapes. In this case, the pulse resolution volume is calculated according to:

V = | π | ·R^{2}· |
c_{0}·τ |
· θ_{az} θ_{el} |
where | c_{0} = speed of light;R _{ } = distance to the radar antenna (range);τ _{ } = duration of the transmitted pulse. |
(2) |

4 | 2 |

In equations (1) and (2) it is assumed that the values of the angles
Θ_{az} and Θ_{el} are given in radians.
If they are in degrees, they should be converted to radians by multiplying by (π/180).

The wider the spectrum of the considered transmit pulse and the narrower the antenna directivity pattern are, the smaller is the pulse resolution volume and the higher is the resolution capability of the radar station. At the same time, the interference immunity from passive disturbances distributed in space (dipole reflectors, ionized clouds, atmospheric structures, fixed targets) increases.

In weather radar, the pulse resolution volume has a greater importance. Since the pulse resolution volume increases with increasing distance, many more raindrops now fit into it for the same rain intensity: the effective reflection area will thus also increase. Therefore, the basic radar equation in weather radar has a completely different form than in an air surveillance radar.

Because of this, in weather radar we also speak of a volume target: the volume target completely fills the pulse resolution volume. In contrast, surveillance radars usually locate point targets: The reflecting object gets lost in the ever increasing pulse resolution volume with increasing distance.

Please do not confuse the pulse resolution volume with the size of a range cell in radar signal processing, i.e. the memory cell corresponding to a range segment. Such range segment should be at most half the size of the pulse resolution volume.

The resolution should also not be confused with accuracy. Nevertheless, in most radar projects, a first guess for the accuracy figure (one standard deviation) will be half the value of the corresponding resolution. When the radar is realized, the accuracy is frequently better than the first guess because: e.g., the range accuracy is a characteristic of the measurement of the elapsed time between the departure of the transmitted pulse and the arrival of the echo at the receiver. If the transmitted pulse is a perfect rectangular one, the received pulse will look like a Gaussian curve because the receiver bandwidth is finite; in addition, the noise will disrupt the Gaussian shape of the received pulse. Hence it is obvious that the accuracy of this measurement is not really linked to the pulse width (which defines the range resolution) but rather on the receiver signal strength (which is linked to the range). Hence the range error should increase with the range.