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NV5 Geospatial Blog

Each month, NV5 Geospatial posts new blog content across a variety of categories. Browse our latest posts below to learn about important geospatial information or use the search bar to find a specific topic or author. Stay informed of the latest blog posts, events, and technologies by joining our email list!



New ENVI Agent, IDL Agent, and GeoAgent Quick Guides

New ENVI Agent, IDL Agent, and GeoAgent Quick Guides

6/9/2026

The recent release of ENVI® Agent, IDL® Agent, and GeoAgent™ revolutionize how users interact with geospatial software. These agentic AI applications act as partners to plan, simplify, and execute complex workflows. Knowing where to start can be challenging for new users. To this end, we developed three new quick guides to... Read More >

Introducing NISAR Data Support

Introducing NISAR Data Support

6/5/2026

The release of ENVI® SARscape 6.3 in April 2026 includes preliminary support for NASA-ISRO SAR (NISAR) data. The NISAR mission is a joint Earth-observing satellite project between NASA and the Indian Space Research Organization designed to monitor changes in the planet’s land and ice surfaces using advanced radar imaging. It... Read More >

Monitoring Illegal Mining in the Amazon: Turning Persistent Data Into Actionable Insight

Monitoring Illegal Mining in the Amazon: Turning Persistent Data Into Actionable Insight

5/28/2026

Illegal mining over decades has constituted one of the most persistent and complex socio-environmental problems in the Brazilian Amazon. In recent years, with the increasingly intensive use of mechanized extraction, the associated environmental impacts—such as deforestation, intense soil disturbance, river siltation, and mercury... Read More >

From Answers to Action: Why ENVI and IDL Agents Go Beyond General AI

From Answers to Action: Why ENVI and IDL Agents Go Beyond General AI

4/20/2026

As generative AI tools like Claude and Gemini continue to gain traction, many organizations are asking the same question: Can general purpose AI actually support real geospatial workflows, or does it stop at surface-level answers? That question was front and center in our recent webinar, Meet Your New Partners in Science: ENVI... Read More >

Mapping Earthquake Deformation in Taiwan With ENVI

Mapping Earthquake Deformation in Taiwan With ENVI

12/15/2025

Unlocking Critical Insights With ENVI® Tools Taiwan sits at the junction of major tectonic plates and regularly experiences powerful earthquakes. Understanding how the ground moves during these events is essential for disaster preparedness, public safety, and building community resilience. But traditional approaches like field... Read More >

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Calculating the period of the sunspot cycle

Anonym

Two weeks ago, I used the sunspot number data provided by the Solar Physics Group at NASA's Marshall Space Flight Center to demonstrate positioning plots in window. This week, I'd like to show how to calculate the period of the sunspot cycle. If you haven't already done so, download the sunspot numbers file and place it in your IDL path. Read it with the astrolib READCOL procedure:

 file = file_which('spot_num.txt', /include) readcol, file, year, month, sunspots

Next, transform the sunspot series to the frequency domain and compute magnitude and power spectra:

 mspec = abs(fft(sunspots)) pspec = mspec^2

(Aside: FFT: it's all you need.) I'd like to display the power spectrum as a function of frequency. This requires a few statements to set up a frequency vector based on the time data from the sunspot numbers file:

 sampling_interval = 1/12.0 ; years, from file freq_nyquist = 0.5/sampling_interval ; years^{-1} n_sunspots = n_elements(sunspots) freq = findgen(n_sunspots/2)/(n_sunspots/2-1)*freq_nyquist

The sampling interval is one month. This allows me to determine the Nyquist frequency (the maximum resolvable frequency), which along with the number of sunspots in the file, gives me the information to define a frequency vector. Note that I'm defining only positive frequencies up to the Nyquist frequency; this is because I'm going to display a one-sided power spectrum. Fold the negative Fourier modes into the spectrum, omitting the zero (DC) mode:

 freq_nodc = freq[1:n_sunspots/2-1] pspec_nodc = 2*pspec[1:n_sunspots/2-1]

and display the result on logarithmic axes:

 p = plot(freq_nodc, pspec_nodc, /xlog, /ylog, $ xtickunits='exponent', $   ; IDL 8.2.1 xtitle='Frequency ($yr^{-1}$)', $ ytitle='Spectral Density', $ title='Power Spectrum of Sunspot Numbers, 1749-2010')

Note that I can set the style of tick units on the axes: 'exponent' and 'scientific' are new in IDL 8.2.1. The power spectrum has a peak near 0.1 yr^{-1}. Locate the peak frequency with MAX and mark it on the plot with POLYLINE:

 pspec_nodc_peak = max(pspec_nodc, i_peak) freq_nodc_peak = freq_nodc[i_peak] !null = polyline([1.0,1.0]*freq_nodc_peak, p.yrange, color='orange', /data)

The inverse of the peak frequency gives the period of the sunspot cycle: approximately 11 years. Mark this on the plot with TEXT:

 sunspot_peak_period = 1.0/freq_nodc_peak str = '$T_{peak}$ = ' + strtrim(sunspot_peak_period,2) + ' years' !null = text(1e-1, 1e-4, str, /data)

Here's my result:

Power spectrum of sunspot numbers time series. Data courtesy NASA.

Finally, just because it's interesting, test Parseval's theorem (energy is conserved in the time- and frequency-domain representations of the signal) in several forms:

 IDL> print, total(pspec)*n_sunspots, total(sunspots^2) 1.46437e+007 1.46437e+007 IDL> print, mspec[0], mean(sunspots) 52.0133      52.0134 IDL> print, total(pspec[1:*]), stddev(sunspots)^2*(n_sunspots-1)/n_sunspots ; convert from sample variance 1965.67      1965.66

Conservation of greatness (of FFT)!

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