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Tests whether continuous frozen / permafrost material occurs within the upper max_top_cm. Two alternative paths qualify per WRB 2022:

  1. Permafrost temperature: a layer at top_cm <= max_top_cm (default 100) with permafrost_temp_C <= max_temp_C (default 0 C).

  2. Designation pattern: a layer at top_cm <= max_top_cm with designation containing suffix "f" (frozen) or matching "^Cf" / "perma". A site that declares the Canadian notation (site$designation_system = "cssc") writes a frozen layer z; the New Zealand and Australian notations have no frozen suffix, so there only "perma" counts. Used as a fallback when the temperature field is not in the pedon (typical of legacy survey data).

Either path qualifies. Diagnostic of Cryosols. When neither passes and the site has a soil temperature regime warmer than gelic (cryic, frigid, mesic, thermic, hyperthermic or an iso form; site$soil_temperature_regime), the answer is no: those regimes have no permafrost (KST 13, Ch. 3, p. 50).

Usage

cryic_conditions(pedon, max_top_cm = 100, max_temp_C = 0)

Arguments

pedon

A PedonRecord.

max_top_cm

Maximum top depth (cm) (default 100).

max_temp_C

Maximum mean annual permafrost-zone temperature (deg C) for the temperature path (default 0).

Value

A DiagnosticResult.

References

IUSS Working Group WRB (2022), Chapter 5, Cryosols.