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energije za duboku konvekciju","desc":"MU paket ima malu energiju. To ne isključuje stratiformne padavine, plitku konvekciju ili kasniju promenu uslova.","confidence":"conditional"},"precip_type":{"type":"rain","label":"Kiša · izvor padavina neizvestan","desc":"Prizemni topli sloj podržava topljenje snega i tečnu fazu pri tlu, ako padavine dospeju do tla. Nije izdvojen pouzdan vlažan izvor; moguće je isparavanje pre tla. Ovaj zaključak opisuje samo uslove za fazu.","status":"limited","reason":"thermal_only_no_moist_source"},"hail":{"category":"weak_signal","label":"Slab signal za značajan grad","size_cm":null,"desc":"SHIP povezuje energiju, vlagu, temperaturu i smicanje. Grad zahteva razvoj odgovarajućeg uzlaznog strujanja; prečnik se ne može pouzdano izvesti iz ovog indeksa. Slab signal ne isključuje sitan grad."},"spc_level":{"level":null,"label":"DIAGNOSTIC","sr_label":"Dijagnostika profila","color":"#2563eb"},"methodology":{"parcel_definition":"SB observed surface; ML mass-mixed 100 hPa; MU max theta-e 300 hPa","effective_layer":"Thompson 2007; 5 hPa search; CAPE >= 100 J/kg, CIN >= -250 J/kg","ship":"SPC/SHARPpy, shear 0-6 km; freezing height MSL","wind":"linear u/v versus observed height; no extrapolation","energy_coverage":"CAPE/CIN withheld when positive buoyancy has no measured EL, or no EL with profile top below 300 hPa","lfc_el":"virtual-temperature intersections, matching MetPy cape_cin integration bounds","surface_tolerance_m":60}}