INGENIA

SRV-03

Position dilution of precision

PDOP ≈ √(σE²+σN²+σU²)/σUERE.

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GNSSGPS ICDIGS

Governing equation

PDOP=σE2+σN2+σU2σUERE\mathrm{PDOP}=\dfrac{\sqrt{\sigma_E^2+\sigma_N^2+\sigma_U^2}}{\sigma_{\mathrm{UERE}}}

σUERE∈[0.2,8]\sigma_{\mathrm{UERE}} \in \left[0.2, 8\right]

where

\sigma_E
East RMS (m)
\sigma_N
North RMS (m)
\sigma_U
Up RMS (m)
\sigma_{\mathrm{UERE}}
UERE (m)
PDOP
PDOP (—)

The figure, part by part

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①

Governing law — red

PDOP=σE2+σN2+σU2σUERE\mathrm{PDOP}=\dfrac{\sqrt{\sigma_E^2+\sigma_N^2+\sigma_U^2}}{\sigma_{\mathrm{UERE}}}

σUERE∈[0.2,8]\sigma_{\mathrm{UERE}} \in \left[0.2, 8\right]

σUERE=0.2\sigma_{\mathrm{UERE}} = 0.2PDOP=14.5PDOP = 14.5

②

Domain of the variable — blue

\sigma_{\mathrm{UERE}}_{\min} = 0.2,\quad \sigma_{\mathrm{UERE}}_{\max} = 8

σUERE∈[0.2,8]\sigma_{\mathrm{UERE}} \in \left[0.2, 8\right]

σUERE=0.2\sigma_{\mathrm{UERE}} = 0.2σUERE=0.2\sigma_{\mathrm{UERE}} = 0.2

③

Response curve — green

PDOP=σE2+σN2+σU2σUERE\mathrm{PDOP}=\dfrac{\sqrt{\sigma_E^2+\sigma_N^2+\sigma_U^2}}{\sigma_{\mathrm{UERE}}}

σUERE∈[0.2,8]\sigma_{\mathrm{UERE}} \in \left[0.2, 8\right]

σUERE=0.2\sigma_{\mathrm{UERE}} = 0.2PDOP=14.5PDOP = 14.5

④

Rate of change — amber

dPDOPdσUERE\frac{\mathrm{d}PDOP}{\mathrm{d}\sigma_{\mathrm{UERE}}}

σUERE∈[0.2,8]\sigma_{\mathrm{UERE}} \in \left[0.2, 8\right]

σUERE=0.249\sigma_{\mathrm{UERE}} = 0.249PDOP′=−48.64PDOP^{\prime} = -48.64

Lecture brief

Historical brief

From chain and theodolite through Bowditch’s compass-rule (1802) to GPS PDOP, surveying is the propagation of small errors across a network. These sheets close traverses, reduce stadia and state map scale. This sheet (SRV-03 — Position dilution of precision) is the form associated with GPS ICD · IGS. Working symbols: σE\sigma_E, σN\sigma_N, σU\sigma_U, σUERE\sigma_{\mathrm{UERE}} →\rightarrow PDOPPDOP. PDOP maps user-equivalent range error onto 3-D position through the geometry matrix (HᵀH)⁻¹.

Purpose

Purpose: compute PDOPPDOP from σE\sigma_E, σN\sigma_N, σU\sigma_U, σUERE\sigma_{\mathrm{UERE}} in Surveying via PDOP=σE2+σN2+σU2σUERE\mathrm{PDOP}=\dfrac{\sqrt{\sigma_E^2+\sigma_N^2+\sigma_U^2}}{\sigma_{\mathrm{UERE}}} PDOP ≈ √(σE²+σN²+σU²)/σUERE. Use it when a real surveying question must be answered in SI before a code check.

Live realistic example

In symbols

Live case. Given σE=1.200 m\sigma_E = 1.200\,\mathrm{m}, σN=1.100 m\sigma_N = 1.100\,\mathrm{m}, σU=2.400 m\sigma_U = 2.400\,\mathrm{m}, σUERE=1.500 m\sigma_{\mathrm{UERE}} = 1.500\,\mathrm{m}, the governing relation PDOP=σE2+σN2+σU2σUERE\mathrm{PDOP}=\dfrac{\sqrt{\sigma_E^2+\sigma_N^2+\sigma_U^2}}{\sigma_{\mathrm{UERE}}} yields PDOP=1.933 —PDOP = 1.933\,\mathrm{—}. Enter component RMS errors and UERE. Pedagogical ratio. Move a slider: the numbers are this situation, not a canned story.

Calculator

Inputs

Outputs

  • PDOP PDOP1.933 —
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Narration of this film

Enter component RMS errors and UERE. Pedagogical ratio.

PDOP maps user-equivalent range error onto 3-D position through the geometry matrix (HᵀH)⁻¹.

Reading speed

Watch on YouTube