For about 75 years, many brilliant minds all over the world have struggled to find a unique solution: one that limits flood-caused damages; a solution that allows the prediction of flash-floods, rainfall caused avalanches and slides; and one that will help thousands of people to survive each year. The way out of the dilemma is to find a correct relation between rainfall and radar reflectivity. However, it is still the most famous, unsolved struggle in radar meteorology.

A radar sends out a pulse of energy and* only *measures the backscattered reflectivity. The Z-R relation is an equation which converts the measured unusable reflectivity *Z* into a quantitative rainfall amount *R*.

It sounds theoretical and rather complicated (and in fact, it’s both), but it is essential for the development of reliable flash-flood warning systems. If the Z-R relation is wrong, either nothing happens and people are wrongly warned, or they are taken by surprise by a rapid moving, devastating wave of muddy water and die. Z-R relations are important, but until now, no effective solution exists to convert the reflectivity to an accurate rain amount.

So what are some of the problems to address?

The first problem is a mathematical one and, sadly, non-fixable. The reflectivity *Z* is a quantity that depends on the sixth power of the rain drop size diameter. The rain amount *R* is a quantity that depends on the third power of the rain drop size diameter. For mathematicians this is a clear case: There is no analytical equation connecting the two quantities *Z* and *R* as long as the raindrop size distribution is not known. And, the raindrop size distribution is highly variable from rain event to rain event. Therefore, most authors use an empirical power function with the form *Z=aR ^{b}* to calculate the rain amount from the measured reflectivity.

The second one is that we only have the one equation *Z=aR ^{b}* with two unknowns

*a*and

*b*. Through experiments it is possible to determine the coefficients

*a*and

*b*. Marshall & Palmer (1948) found the relation

*Z=200R*with the parameters

^{1.6}*a=200*and

*b=1.6*, which is widely used, among others, also by the Meteorological Office in Norway (MET.no).

The third problem – and it matters now – is that the parameters *a* and *b* are used operationally as constants, but actually vary strongly from one rain event to another. Within one hour, the parameter *a* can easily vary between *100* and *300*. And in fact, the parameters depend on atmospheric conditions, on the geographic locality, and on the rain type. A wrong parameter *a*, and the calculated rain rate is *200 %* higher or lower than it actually should be.

A so called Micro Rain Radar (MRR) can provide a solution to the still unsolved Z-R problem, since it provides Z-R relations in nearly real-time. If you ask me, to solve the Z-R problem, two or three Micro Rain Radars for every operational weather radar are the way to go. With these real-time radars, the hydrological models receive the necessary input. As a result, flood or flash-flood forecasting will be improved. The geographical position of hydropower plants can be optimized. Buildings and roads could be made flood resistant. All these benefits are given by operating some supportive Micro Rain Radars.

In 2015, Norway lost about 51 Million Euros because of flood damages and not less in the previous years (NASK – Norsk Naturskadepool).

Could this problem be avoided in the future with Micro Rain Radars?

Absolutely.

**References:**

Marshall, J. S., and W. McK. Palmer 1948. The distribution of raindrops with size. J. Meteor.. 5. 165–166.