"pipkrake" meaning in English

{
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        "2": "sv",
        "3": "pipkrake"
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      "expansion": "Swedish pipkrake",
      "name": "bor"
    },
    {
      "args": {
        "1": "sv",
        "2": "pip",
        "3": "krake",
        "nocat": "1",
        "t1": "tube",
        "t2": "thin, fine, weak"
      },
      "expansion": "pip (“tube”) + krake (“thin, fine, weak”)",
      "name": "af"
    },
    {
      "args": {
        "1": "sv",
        "2": "Henrik Hesselman",
        "in": "1907",
        "nat": "Swedish",
        "nocap": "1",
        "nocat": "1",
        "occ": "botanist"
      },
      "expansion": "coined by Swedish botanist Henrik Hesselman in 1907",
      "name": "coin"
    }
  ],
  "etymology_text": "From Swedish pipkrake, from pip (“tube”) + krake (“thin, fine, weak”), coined by Swedish botanist Henrik Hesselman in 1907.",
  "forms": [
    {
      "form": "pipkrakes",
      "tags": [
        "plural"
      ]
    }
  ],
  "head_templates": [
    {
      "args": {
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      },
      "expansion": "pipkrake (countable and uncountable, plural pipkrakes)",
      "name": "en-noun"
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  ],
  "lang": "English",
  "lang_code": "en",
  "pos": "noun",
  "senses": [
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          "kind": "other",
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          "source": "w"
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          "parents": [],
          "source": "w"
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      ],
      "examples": [
        {
          "ref": "1979, E. Derbyshire, Geomorphological Processes, Routledge, →ISBN, page 208:",
          "text": "The most widespread and familiar example of this process is that associated with the growth of needle ice or pipkrake (Figure 5.15), needles of clear ice commonly exceeding 5 cm in length. Growth of pipkrake is favoured by supercooling of the soil in conditions of marked radiative heat loss from the surface […]",
          "type": "quote"
        }
      ],
      "glosses": [
        "Needle ice; ice structures formed when the air temperature is below 0℃ and the soil is not."
      ],
      "id": "en-pipkrake-en-noun-kS4sEFlz",
      "tags": [
        "countable",
        "uncountable"
      ]
    }
  ],
  "word": "pipkrake"
}

{
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    {
      "args": {
        "1": "en",
        "2": "sv",
        "3": "pipkrake"
      },
      "expansion": "Swedish pipkrake",
      "name": "bor"
    },
    {
      "args": {
        "1": "sv",
        "2": "pip",
        "3": "krake",
        "nocat": "1",
        "t1": "tube",
        "t2": "thin, fine, weak"
      },
      "expansion": "pip (“tube”) + krake (“thin, fine, weak”)",
      "name": "af"
    },
    {
      "args": {
        "1": "sv",
        "2": "Henrik Hesselman",
        "in": "1907",
        "nat": "Swedish",
        "nocap": "1",
        "nocat": "1",
        "occ": "botanist"
      },
      "expansion": "coined by Swedish botanist Henrik Hesselman in 1907",
      "name": "coin"
    }
  ],
  "etymology_text": "From Swedish pipkrake, from pip (“tube”) + krake (“thin, fine, weak”), coined by Swedish botanist Henrik Hesselman in 1907.",
  "forms": [
    {
      "form": "pipkrakes",
      "tags": [
        "plural"
      ]
    }
  ],
  "head_templates": [
    {
      "args": {
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      "expansion": "pipkrake (countable and uncountable, plural pipkrakes)",
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  "lang": "English",
  "lang_code": "en",
  "pos": "noun",
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      "examples": [
        {
          "ref": "1979, E. Derbyshire, Geomorphological Processes, Routledge, →ISBN, page 208:",
          "text": "The most widespread and familiar example of this process is that associated with the growth of needle ice or pipkrake (Figure 5.15), needles of clear ice commonly exceeding 5 cm in length. Growth of pipkrake is favoured by supercooling of the soil in conditions of marked radiative heat loss from the surface […]",
          "type": "quote"
        }
      ],
      "glosses": [
        "Needle ice; ice structures formed when the air temperature is below 0℃ and the soil is not."
      ],
      "tags": [
        "countable",
        "uncountable"
      ]
    }
  ],
  "word": "pipkrake"
}