NA; paleoData_inferredMaterial has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized
NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized
NA; paleoData_isPrimary has been standardized
The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.
NA; paleoData_inferredMaterial has been standardized
Marked in original compilation as primary P timeseries; Pass age control and data resolution; pvalue <0.1
originalDataUrl: 'https://doi.pangaea.de/10.1594/PANGAEA.930512' has been replaced by 'https://doi.org/10.1594/10.1594/PANGAEA.930512'
precipitation (lcRBEvaydIFwOnSZuma): interpretation1_variableDetail: 'precipitation@surface' has been replaced by 'amount@surface'
Updated lipdverse database entry with a changed file.
geo_elevation: '' has been replaced by '1000'
uncertaintyHigh (lcRBe6MA38yyyZF7q3S): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyLow (lcRcfqHRUf3HJKYVf6D): interpretation1_scope: '' has been replaced by 'climate'
precipitation (lcRBEvaydIFwOnSZuma): paleoData_notes: '' has been replaced by 'null'
precipitation (lcRcxrVNR2nWomdDibe): paleoData_notes: '' has been replaced by 'null'
precipitation (lcRDLIrQ3r1bza10EP1): paleoData_notes: '' has been replaced by 'null'
precipitation (lcRey1szXCIV3MDlOQu): paleoData_notes: '' has been replaced by 'null'
precipitation (lcRH5hdhvPNova4q7T8): paleoData_notes: '' has been replaced by 'null'
archiveType: 'Lake' has been replaced by 'LakeSediment'
age (lcR0t3sAT5szANuEclS): paleoData_datum: '' has been replaced by '1950'
age (lcR0t3sAT5szANuEclS): paleoData_variableName: 'ageMedian' has been replaced by 'age'
age (lcR0t3sAT5szANuEclS): paleoData_isPrimary: '' has been replaced by 'FALSE'
age (lcR0t3sAT5szANuEclS): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
depth (lcR0z6byeKnomhjv1tx): paleoData_isPrimary: '' has been replaced by 'TRUE'
depth (lcR0z6byeKnomhjv1tx): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized'
age (lcR9LOURf4cVBkltT1v): paleoData_datum: '' has been replaced by '1950'
age (lcR9LOURf4cVBkltT1v): paleoData_isPrimary: '' has been replaced by 'TRUE'
age (lcR9LOURf4cVBkltT1v): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
uncertainty (lcRaBtvhnbXzd6pYLOD): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
uncertainty (lcRaBtvhnbXzd6pYLOD): paleoData_inferredMaterial: '' has been replaced by 'temperature'
uncertainty (lcRaBtvhnbXzd6pYLOD): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
uncertainty (lcRACZZn67ECABJEqIp): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
uncertainty (lcRACZZn67ECABJEqIp): paleoData_variableName: 'precipitationUncertainty' has been replaced by 'uncertainty'
uncertainty (lcRACZZn67ECABJEqIp): paleoData_inferredMaterial: '' has been replaced by 'precipitation'
uncertainty (lcRACZZn67ECABJEqIp): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
uncertaintyHigh (lcRBe6MA38yyyZF7q3S): paleoData_datum: '' has been replaced by '1950'
uncertaintyHigh (lcRBe6MA38yyyZF7q3S): paleoData_variableName: 'ageMax' has been replaced by 'uncertaintyHigh'
uncertaintyHigh (lcRBe6MA38yyyZF7q3S): paleoData_isPrimary: '' has been replaced by 'FALSE'
uncertaintyHigh (lcRBe6MA38yyyZF7q3S): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
precipitation (lcRBEvaydIFwOnSZuma): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
uncertaintyLow (lcRcfqHRUf3HJKYVf6D): paleoData_datum: '' has been replaced by '1950'
uncertaintyLow (lcRcfqHRUf3HJKYVf6D): paleoData_variableName: 'ageMin' has been replaced by 'uncertaintyLow'
uncertaintyLow (lcRcfqHRUf3HJKYVf6D): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyLow (lcRcfqHRUf3HJKYVf6D): paleoData_isPrimary: '' has been replaced by 'FALSE'
uncertaintyLow (lcRcfqHRUf3HJKYVf6D): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
precipitation (lcRcxrVNR2nWomdDibe): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
precipitation (lcRDLIrQ3r1bza10EP1): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
uncertainty (lcRdtbiak4cBS9UNCl2): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
uncertainty (lcRdtbiak4cBS9UNCl2): paleoData_variableName: 'precipitationUncertainty' has been replaced by 'uncertainty'
uncertainty (lcRdtbiak4cBS9UNCl2): paleoData_inferredMaterial: '' has been replaced by 'precipitation'
uncertainty (lcRdtbiak4cBS9UNCl2): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
precipitation (lcRey1szXCIV3MDlOQu): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
uncertainty (lcRFSEF4OL5Vk4jFuIE): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
uncertainty (lcRFSEF4OL5Vk4jFuIE): paleoData_variableName: 'precipitationUncertainty' has been replaced by 'uncertainty'
uncertainty (lcRFSEF4OL5Vk4jFuIE): paleoData_inferredMaterial: '' has been replaced by 'precipitation'
uncertainty (lcRFSEF4OL5Vk4jFuIE): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
uncertainty (lcRg28xetE4FcERjdJy): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
uncertainty (lcRg28xetE4FcERjdJy): paleoData_inferredMaterial: '' has been replaced by 'temperature'
uncertainty (lcRg28xetE4FcERjdJy): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
precipitation (lcRH5hdhvPNova4q7T8): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
uncertainty (lcRKnRU8BaG89LhHfcI): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
uncertainty (lcRKnRU8BaG89LhHfcI): paleoData_inferredMaterial: '' has been replaced by 'temperature'
uncertainty (lcRKnRU8BaG89LhHfcI): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
uncertainty (lcRkPFrIQCjycIWczXz): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
uncertainty (lcRkPFrIQCjycIWczXz): paleoData_inferredMaterial: '' has been replaced by 'temperature'
uncertainty (lcRkPFrIQCjycIWczXz): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
uncertainty (lcRloO7sekK2UgRzAN6): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
uncertainty (lcRloO7sekK2UgRzAN6): paleoData_inferredMaterial: '' has been replaced by 'temperature'
uncertainty (lcRloO7sekK2UgRzAN6): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
uncertainty (lcRoeTZpvXUXQDYJbUW): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
uncertainty (lcRoeTZpvXUXQDYJbUW): paleoData_inferredMaterial: '' has been replaced by 'temperature'
uncertainty (lcRoeTZpvXUXQDYJbUW): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
uncertainty (lcRt2tvSndxaHJf95q1): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
uncertainty (lcRt2tvSndxaHJf95q1): paleoData_variableName: 'precipitationUncertainty' has been replaced by 'uncertainty'
uncertainty (lcRt2tvSndxaHJf95q1): paleoData_inferredMaterial: '' has been replaced by 'precipitation'
uncertainty (lcRt2tvSndxaHJf95q1): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
uncertainty (lcRxyCa4XQKzGKkEceF): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
uncertainty (lcRxyCa4XQKzGKkEceF): paleoData_inferredMaterial: '' has been replaced by 'temperature'
uncertainty (lcRxyCa4XQKzGKkEceF): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
uncertainty (lcRyZkdjY6gA9pvlIdZ): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
uncertainty (lcRyZkdjY6gA9pvlIdZ): paleoData_inferredMaterial: '' has been replaced by 'temperature'
uncertainty (lcRyZkdjY6gA9pvlIdZ): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
uncertainty (lcRz8WFv2GH7NS4KdOU): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
uncertainty (lcRz8WFv2GH7NS4KdOU): paleoData_variableName: 'precipitationUncertainty' has been replaced by 'uncertainty'
uncertainty (lcRz8WFv2GH7NS4KdOU): paleoData_inferredMaterial: '' has been replaced by 'precipitation'
uncertainty (lcRz8WFv2GH7NS4KdOU): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
temperature (lcR7wdiBBdrwSVan3v6): interpretation1_variable: 'T' has been replaced by 'temperature'
temperature (lcRAaspP4ZPsRPpNmK3): interpretation1_variable: 'T' has been replaced by 'temperature'
uncertainty (lcRaBtvhnbXzd6pYLOD): interpretation1_seasonality: 'July' has been replaced by 'Jul'
uncertainty (lcRaBtvhnbXzd6pYLOD): interpretation1_variable: 'T' has been replaced by 'temperature'
uncertainty (lcRACZZn67ECABJEqIp): interpretation1_variable: 'P' has been replaced by 'precipitation'
precipitation (lcRBEvaydIFwOnSZuma): interpretation1_seasonality: '1,2,3,4,5,6,7,8,9,10,11,12' has been replaced by 'Annual'
precipitation (lcRBEvaydIFwOnSZuma): interpretation1_variable: 'P' has been replaced by 'precipitation'
temperature (lcRBUQS8kdbl9IOGHfr): interpretation1_seasonality: 'July' has been replaced by 'Jul'
temperature (lcRBUQS8kdbl9IOGHfr): interpretation1_variable: 'T' has been replaced by 'temperature'
precipitation (lcRcxrVNR2nWomdDibe): interpretation1_variable: 'P' has been replaced by 'precipitation'
precipitation (lcRDLIrQ3r1bza10EP1): interpretation1_variable: 'P' has been replaced by 'precipitation'
temperature (lcRDsQI4d9Vj9NmLyO4): interpretation1_seasonality: 'July' has been replaced by 'Jul'
temperature (lcRDsQI4d9Vj9NmLyO4): interpretation1_variable: 'T' has been replaced by 'temperature'
uncertainty (lcRdtbiak4cBS9UNCl2): interpretation1_variable: 'P' has been replaced by 'precipitation'
precipitation (lcRey1szXCIV3MDlOQu): interpretation1_variable: 'P' has been replaced by 'precipitation'
uncertainty (lcRFSEF4OL5Vk4jFuIE): interpretation1_variable: 'P' has been replaced by 'precipitation'
uncertainty (lcRg28xetE4FcERjdJy): interpretation1_variable: 'T' has been replaced by 'temperature'
precipitation (lcRH5hdhvPNova4q7T8): interpretation1_variable: 'P' has been replaced by 'precipitation'
uncertainty (lcRKnRU8BaG89LhHfcI): interpretation1_variable: 'T' has been replaced by 'temperature'
uncertainty (lcRkPFrIQCjycIWczXz): interpretation1_seasonality: 'July' has been replaced by 'Jul'
uncertainty (lcRkPFrIQCjycIWczXz): interpretation1_variable: 'T' has been replaced by 'temperature'
temperature (lcRkWs33uxYMlG8FERV): interpretation1_seasonality: 'July' has been replaced by 'Jul'
temperature (lcRkWs33uxYMlG8FERV): interpretation1_variable: 'T' has been replaced by 'temperature'
uncertainty (lcRloO7sekK2UgRzAN6): interpretation1_variable: 'T' has been replaced by 'temperature'
uncertainty (lcRoeTZpvXUXQDYJbUW): interpretation1_seasonality: 'July' has been replaced by 'Jul'
uncertainty (lcRoeTZpvXUXQDYJbUW): interpretation1_variable: 'T' has been replaced by 'temperature'
temperature (lcRqPq0E2ipc9svss1o): interpretation1_variable: 'T' has been replaced by 'temperature'
uncertainty (lcRt2tvSndxaHJf95q1): interpretation1_variable: 'P' has been replaced by 'precipitation'
temperature (lcRut4aNuph5mDCCvOM): interpretation1_seasonality: 'July' has been replaced by 'Jul'
temperature (lcRut4aNuph5mDCCvOM): interpretation1_variable: 'T' has been replaced by 'temperature'
temperature (lcRXwlNyww6riv4ygrW): interpretation1_variable: 'T' has been replaced by 'temperature'
uncertainty (lcRxyCa4XQKzGKkEceF): interpretation1_variable: 'T' has been replaced by 'temperature'
uncertainty (lcRyZkdjY6gA9pvlIdZ): interpretation1_seasonality: 'July' has been replaced by 'Jul'
uncertainty (lcRyZkdjY6gA9pvlIdZ): interpretation1_variable: 'T' has been replaced by 'temperature'
uncertainty (lcRz8WFv2GH7NS4KdOU): interpretation1_variable: 'P' has been replaced by 'precipitation'
precipitation (lcRBEvaydIFwOnSZuma): paleoData_QCnotes: 'Marked in original compilation as primary P timeseries; Pass age control and data resolution' has been replaced by 'Marked in original compilation as primary P timeseries; Pass age control and data resolution; pvalue <0.1'
precipitation (lcRBEvaydIFwOnSZuma): interpretation1_seasonality: 'Annual' has been replaced by '1,2,3,4,5,6,7,8,9,10,11,12'
originalDataUrl: '' has been replaced by 'https://doi.pangaea.de/10.1594/PANGAEA.930512'
pub1_year: '' has been replaced by '2009'
pub1_author: '' has been replaced by 'Ravindra, R.'
pub1_doi: '' has been replaced by 'Ravindra, R., 2009. A high-resolution vegetation, fire, and climate history from the Aishihik Region, Yukon Territory, Canada. Master's thesis. University of Ottawa, Ottawa, Ontario, Canada.'
pub1_journal: '' has been replaced by 'Master's thesis. University of Ottawa'
pub1_title: '' has been replaced by 'A high-resolution vegetation, fire, and climate history from the Aishihik Region, Yukon Territory, Canada.'
pub2_doi: '' has been replaced by '10.5194/essd-2022-38'
geo_elevation: '1000' has been replaced by ''
geo_gcmdLocation: '' has been replaced by 'North America>Canada>Yukon Territory'
temperature (lcR7wdiBBdrwSVan3v6): paleoData_datum: '' has been replaced by 'abs'
temperature (lcR7wdiBBdrwSVan3v6): paleoData_proxy: '' has been replaced by 'pollen'
temperature (lcR7wdiBBdrwSVan3v6): paleoData_proxyDetail: '' has been replaced by 'The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.'
temperature (lcR7wdiBBdrwSVan3v6): paleoData_proxyGeneral: '' has been replaced by 'pollen'
temperature (lcRAaspP4ZPsRPpNmK3): paleoData_datum: '' has been replaced by 'abs'
temperature (lcRAaspP4ZPsRPpNmK3): paleoData_proxy: '' has been replaced by 'pollen'
temperature (lcRAaspP4ZPsRPpNmK3): paleoData_proxyDetail: '' has been replaced by 'The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.'
temperature (lcRAaspP4ZPsRPpNmK3): paleoData_proxyGeneral: '' has been replaced by 'pollen'
temperatureUncertainty (lcRaBtvhnbXzd6pYLOD): paleoData_datum: '' has been replaced by 'abs'
temperatureUncertainty (lcRaBtvhnbXzd6pYLOD): paleoData_proxy: '' has been replaced by 'pollen'
temperatureUncertainty (lcRaBtvhnbXzd6pYLOD): paleoData_proxyDetail: '' has been replaced by 'The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.'
temperatureUncertainty (lcRaBtvhnbXzd6pYLOD): paleoData_proxyGeneral: '' has been replaced by 'pollen'
precipitationUncertainty (lcRACZZn67ECABJEqIp): paleoData_datum: '' has been replaced by 'abs'
precipitationUncertainty (lcRACZZn67ECABJEqIp): paleoData_proxy: '' has been replaced by 'pollen'
precipitationUncertainty (lcRACZZn67ECABJEqIp): paleoData_proxyDetail: '' has been replaced by 'The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.'
precipitationUncertainty (lcRACZZn67ECABJEqIp): paleoData_proxyGeneral: '' has been replaced by 'pollen'
precipitation (lcRBEvaydIFwOnSZuma): paleoData_datum: '' has been replaced by 'abs'
precipitation (lcRBEvaydIFwOnSZuma): paleoData_proxy: '' has been replaced by 'pollen'
precipitation (lcRBEvaydIFwOnSZuma): paleoData_proxyDetail: '' has been replaced by 'The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.'
precipitation (lcRBEvaydIFwOnSZuma): paleoData_proxyGeneral: '' has been replaced by 'pollen'
precipitation (lcRBEvaydIFwOnSZuma): paleoData_QCCertification: '' has been replaced by 'CH'
precipitation (lcRBEvaydIFwOnSZuma): paleoData_QCnotes: '' has been replaced by 'Marked in original compilation as primary P timeseries; Pass age control and data resolution'
temperature (lcRBUQS8kdbl9IOGHfr): paleoData_datum: '' has been replaced by 'abs'
temperature (lcRBUQS8kdbl9IOGHfr): paleoData_proxy: '' has been replaced by 'pollen'
temperature (lcRBUQS8kdbl9IOGHfr): paleoData_proxyDetail: '' has been replaced by 'The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.'
temperature (lcRBUQS8kdbl9IOGHfr): paleoData_proxyGeneral: '' has been replaced by 'pollen'
precipitation (lcRcxrVNR2nWomdDibe): paleoData_datum: '' has been replaced by 'abs'
precipitation (lcRcxrVNR2nWomdDibe): paleoData_proxy: '' has been replaced by 'pollen'
precipitation (lcRcxrVNR2nWomdDibe): paleoData_proxyDetail: '' has been replaced by 'The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.'
precipitation (lcRcxrVNR2nWomdDibe): paleoData_proxyGeneral: '' has been replaced by 'pollen'
precipitation (lcRDLIrQ3r1bza10EP1): paleoData_datum: '' has been replaced by 'abs'
precipitation (lcRDLIrQ3r1bza10EP1): paleoData_proxy: '' has been replaced by 'pollen'
precipitation (lcRDLIrQ3r1bza10EP1): paleoData_proxyDetail: '' has been replaced by 'The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.'
precipitation (lcRDLIrQ3r1bza10EP1): paleoData_proxyGeneral: '' has been replaced by 'pollen'
temperature (lcRDsQI4d9Vj9NmLyO4): paleoData_datum: '' has been replaced by 'abs'
temperature (lcRDsQI4d9Vj9NmLyO4): paleoData_proxy: '' has been replaced by 'pollen'
temperature (lcRDsQI4d9Vj9NmLyO4): paleoData_proxyDetail: '' has been replaced by 'The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.'
temperature (lcRDsQI4d9Vj9NmLyO4): paleoData_proxyGeneral: '' has been replaced by 'pollen'
precipitationUncertainty (lcRdtbiak4cBS9UNCl2): paleoData_datum: '' has been replaced by 'abs'
precipitationUncertainty (lcRdtbiak4cBS9UNCl2): paleoData_proxy: '' has been replaced by 'pollen'
precipitationUncertainty (lcRdtbiak4cBS9UNCl2): paleoData_proxyDetail: '' has been replaced by 'The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.'
precipitationUncertainty (lcRdtbiak4cBS9UNCl2): paleoData_proxyGeneral: '' has been replaced by 'pollen'
precipitation (lcRey1szXCIV3MDlOQu): paleoData_datum: '' has been replaced by 'abs'
precipitation (lcRey1szXCIV3MDlOQu): paleoData_proxy: '' has been replaced by 'pollen'
precipitation (lcRey1szXCIV3MDlOQu): paleoData_proxyDetail: '' has been replaced by 'The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.'
precipitation (lcRey1szXCIV3MDlOQu): paleoData_proxyGeneral: '' has been replaced by 'pollen'
precipitationUncertainty (lcRFSEF4OL5Vk4jFuIE): paleoData_datum: '' has been replaced by 'abs'
precipitationUncertainty (lcRFSEF4OL5Vk4jFuIE): paleoData_proxy: '' has been replaced by 'pollen'
precipitationUncertainty (lcRFSEF4OL5Vk4jFuIE): paleoData_proxyDetail: '' has been replaced by 'The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.'
precipitationUncertainty (lcRFSEF4OL5Vk4jFuIE): paleoData_proxyGeneral: '' has been replaced by 'pollen'
temperatureUncertainty (lcRg28xetE4FcERjdJy): paleoData_datum: '' has been replaced by 'abs'
temperatureUncertainty (lcRg28xetE4FcERjdJy): paleoData_proxy: '' has been replaced by 'pollen'
temperatureUncertainty (lcRg28xetE4FcERjdJy): paleoData_proxyDetail: '' has been replaced by 'The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.'
temperatureUncertainty (lcRg28xetE4FcERjdJy): paleoData_proxyGeneral: '' has been replaced by 'pollen'
precipitation (lcRH5hdhvPNova4q7T8): paleoData_datum: '' has been replaced by 'abs'
precipitation (lcRH5hdhvPNova4q7T8): paleoData_proxy: '' has been replaced by 'pollen'
precipitation (lcRH5hdhvPNova4q7T8): paleoData_proxyDetail: '' has been replaced by 'The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.'
precipitation (lcRH5hdhvPNova4q7T8): paleoData_proxyGeneral: '' has been replaced by 'pollen'
temperatureUncertainty (lcRKnRU8BaG89LhHfcI): paleoData_datum: '' has been replaced by 'abs'
temperatureUncertainty (lcRKnRU8BaG89LhHfcI): paleoData_proxy: '' has been replaced by 'pollen'
temperatureUncertainty (lcRKnRU8BaG89LhHfcI): paleoData_proxyDetail: '' has been replaced by 'The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.'
temperatureUncertainty (lcRKnRU8BaG89LhHfcI): paleoData_proxyGeneral: '' has been replaced by 'pollen'
temperatureUncertainty (lcRkPFrIQCjycIWczXz): paleoData_datum: '' has been replaced by 'abs'
temperatureUncertainty (lcRkPFrIQCjycIWczXz): paleoData_proxy: '' has been replaced by 'pollen'
temperatureUncertainty (lcRkPFrIQCjycIWczXz): paleoData_proxyDetail: '' has been replaced by 'The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.'
temperatureUncertainty (lcRkPFrIQCjycIWczXz): paleoData_proxyGeneral: '' has been replaced by 'pollen'
temperature (lcRkWs33uxYMlG8FERV): paleoData_datum: '' has been replaced by 'abs'
temperature (lcRkWs33uxYMlG8FERV): paleoData_proxy: '' has been replaced by 'pollen'
temperature (lcRkWs33uxYMlG8FERV): paleoData_proxyDetail: '' has been replaced by 'The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.'
temperature (lcRkWs33uxYMlG8FERV): paleoData_proxyGeneral: '' has been replaced by 'pollen'
temperatureUncertainty (lcRloO7sekK2UgRzAN6): paleoData_datum: '' has been replaced by 'abs'
temperatureUncertainty (lcRloO7sekK2UgRzAN6): paleoData_proxy: '' has been replaced by 'pollen'
temperatureUncertainty (lcRloO7sekK2UgRzAN6): paleoData_proxyDetail: '' has been replaced by 'The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.'
temperatureUncertainty (lcRloO7sekK2UgRzAN6): paleoData_proxyGeneral: '' has been replaced by 'pollen'
temperatureUncertainty (lcRoeTZpvXUXQDYJbUW): paleoData_datum: '' has been replaced by 'abs'
temperatureUncertainty (lcRoeTZpvXUXQDYJbUW): paleoData_proxy: '' has been replaced by 'pollen'
temperatureUncertainty (lcRoeTZpvXUXQDYJbUW): paleoData_proxyDetail: '' has been replaced by 'The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.'
temperatureUncertainty (lcRoeTZpvXUXQDYJbUW): paleoData_proxyGeneral: '' has been replaced by 'pollen'
temperature (lcRqPq0E2ipc9svss1o): paleoData_datum: '' has been replaced by 'abs'
temperature (lcRqPq0E2ipc9svss1o): paleoData_proxy: '' has been replaced by 'pollen'
temperature (lcRqPq0E2ipc9svss1o): paleoData_proxyDetail: '' has been replaced by 'The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.'
temperature (lcRqPq0E2ipc9svss1o): paleoData_proxyGeneral: '' has been replaced by 'pollen'
precipitationUncertainty (lcRt2tvSndxaHJf95q1): paleoData_datum: '' has been replaced by 'abs'
precipitationUncertainty (lcRt2tvSndxaHJf95q1): paleoData_proxy: '' has been replaced by 'pollen'
precipitationUncertainty (lcRt2tvSndxaHJf95q1): paleoData_proxyDetail: '' has been replaced by 'The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.'
precipitationUncertainty (lcRt2tvSndxaHJf95q1): paleoData_proxyGeneral: '' has been replaced by 'pollen'
temperature (lcRut4aNuph5mDCCvOM): paleoData_datum: '' has been replaced by 'abs'
temperature (lcRut4aNuph5mDCCvOM): paleoData_proxy: '' has been replaced by 'pollen'
temperature (lcRut4aNuph5mDCCvOM): paleoData_proxyDetail: '' has been replaced by 'The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.'
temperature (lcRut4aNuph5mDCCvOM): paleoData_proxyGeneral: '' has been replaced by 'pollen'
temperature (lcRXwlNyww6riv4ygrW): paleoData_datum: '' has been replaced by 'abs'
temperature (lcRXwlNyww6riv4ygrW): paleoData_proxy: '' has been replaced by 'pollen'
temperature (lcRXwlNyww6riv4ygrW): paleoData_proxyDetail: '' has been replaced by 'The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.'
temperature (lcRXwlNyww6riv4ygrW): paleoData_proxyGeneral: '' has been replaced by 'pollen'
temperatureUncertainty (lcRxyCa4XQKzGKkEceF): paleoData_datum: '' has been replaced by 'abs'
temperatureUncertainty (lcRxyCa4XQKzGKkEceF): paleoData_proxy: '' has been replaced by 'pollen'
temperatureUncertainty (lcRxyCa4XQKzGKkEceF): paleoData_proxyDetail: '' has been replaced by 'The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.'
temperatureUncertainty (lcRxyCa4XQKzGKkEceF): paleoData_proxyGeneral: '' has been replaced by 'pollen'
temperatureUncertainty (lcRyZkdjY6gA9pvlIdZ): paleoData_datum: '' has been replaced by 'abs'
temperatureUncertainty (lcRyZkdjY6gA9pvlIdZ): paleoData_proxy: '' has been replaced by 'pollen'
temperatureUncertainty (lcRyZkdjY6gA9pvlIdZ): paleoData_proxyDetail: '' has been replaced by 'The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.'
temperatureUncertainty (lcRyZkdjY6gA9pvlIdZ): paleoData_proxyGeneral: '' has been replaced by 'pollen'
precipitationUncertainty (lcRz8WFv2GH7NS4KdOU): paleoData_datum: '' has been replaced by 'abs'
precipitationUncertainty (lcRz8WFv2GH7NS4KdOU): paleoData_proxy: '' has been replaced by 'pollen'
precipitationUncertainty (lcRz8WFv2GH7NS4KdOU): paleoData_proxyDetail: '' has been replaced by 'The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.'
precipitationUncertainty (lcRz8WFv2GH7NS4KdOU): paleoData_proxyGeneral: '' has been replaced by 'pollen'
temperature (lcR7wdiBBdrwSVan3v6): interpretation1_direction: '' has been replaced by 'positive'
temperature (lcR7wdiBBdrwSVan3v6): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'
temperature (lcRAaspP4ZPsRPpNmK3): interpretation1_direction: '' has been replaced by 'positive'
temperature (lcRAaspP4ZPsRPpNmK3): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'
temperatureUncertainty (lcRaBtvhnbXzd6pYLOD): interpretation1_direction: '' has been replaced by 'positive'
temperatureUncertainty (lcRaBtvhnbXzd6pYLOD): interpretation1_seasonalityGeneral: '' has been replaced by 'summer+'
precipitationUncertainty (lcRACZZn67ECABJEqIp): interpretation1_variableDetail: 'precip@surface' has been replaced by 'precipitation@surface'
precipitationUncertainty (lcRACZZn67ECABJEqIp): interpretation1_direction: '' has been replaced by 'positive'
precipitationUncertainty (lcRACZZn67ECABJEqIp): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'
precipitation (lcRBEvaydIFwOnSZuma): interpretation1_variableDetail: 'precip@surface' has been replaced by 'precipitation@surface'
precipitation (lcRBEvaydIFwOnSZuma): interpretation1_direction: '' has been replaced by 'positive'
precipitation (lcRBEvaydIFwOnSZuma): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'
temperature (lcRBUQS8kdbl9IOGHfr): interpretation1_direction: '' has been replaced by 'positive'
temperature (lcRBUQS8kdbl9IOGHfr): interpretation1_seasonalityGeneral: '' has been replaced by 'summer+'
precipitation (lcRcxrVNR2nWomdDibe): interpretation1_variableDetail: 'precip@surface' has been replaced by 'precipitation@surface'
precipitation (lcRcxrVNR2nWomdDibe): interpretation1_direction: '' has been replaced by 'positive'
precipitation (lcRcxrVNR2nWomdDibe): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'
precipitation (lcRDLIrQ3r1bza10EP1): interpretation1_variableDetail: 'precip@surface' has been replaced by 'precipitation@surface'
precipitation (lcRDLIrQ3r1bza10EP1): interpretation1_direction: '' has been replaced by 'positive'
precipitation (lcRDLIrQ3r1bza10EP1): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'
temperature (lcRDsQI4d9Vj9NmLyO4): interpretation1_direction: '' has been replaced by 'positive'
temperature (lcRDsQI4d9Vj9NmLyO4): interpretation1_seasonalityGeneral: '' has been replaced by 'summer+'
precipitationUncertainty (lcRdtbiak4cBS9UNCl2): interpretation1_variableDetail: 'precip@surface' has been replaced by 'precipitation@surface'
precipitationUncertainty (lcRdtbiak4cBS9UNCl2): interpretation1_direction: '' has been replaced by 'positive'
precipitationUncertainty (lcRdtbiak4cBS9UNCl2): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'
precipitation (lcRey1szXCIV3MDlOQu): interpretation1_variableDetail: 'precip@surface' has been replaced by 'precipitation@surface'
precipitation (lcRey1szXCIV3MDlOQu): interpretation1_direction: '' has been replaced by 'positive'
precipitation (lcRey1szXCIV3MDlOQu): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'
precipitationUncertainty (lcRFSEF4OL5Vk4jFuIE): interpretation1_variableDetail: 'precip@surface' has been replaced by 'precipitation@surface'
precipitationUncertainty (lcRFSEF4OL5Vk4jFuIE): interpretation1_direction: '' has been replaced by 'positive'
precipitationUncertainty (lcRFSEF4OL5Vk4jFuIE): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'
temperatureUncertainty (lcRg28xetE4FcERjdJy): interpretation1_direction: '' has been replaced by 'positive'
temperatureUncertainty (lcRg28xetE4FcERjdJy): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'
precipitation (lcRH5hdhvPNova4q7T8): interpretation1_variableDetail: 'precip@surface' has been replaced by 'precipitation@surface'
precipitation (lcRH5hdhvPNova4q7T8): interpretation1_direction: '' has been replaced by 'positive'
precipitation (lcRH5hdhvPNova4q7T8): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'
temperatureUncertainty (lcRKnRU8BaG89LhHfcI): interpretation1_direction: '' has been replaced by 'positive'
temperatureUncertainty (lcRKnRU8BaG89LhHfcI): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'
temperatureUncertainty (lcRkPFrIQCjycIWczXz): interpretation1_direction: '' has been replaced by 'positive'
temperatureUncertainty (lcRkPFrIQCjycIWczXz): interpretation1_seasonalityGeneral: '' has been replaced by 'summer+'
temperature (lcRkWs33uxYMlG8FERV): interpretation1_direction: '' has been replaced by 'positive'
temperature (lcRkWs33uxYMlG8FERV): interpretation1_seasonalityGeneral: '' has been replaced by 'summer+'
temperatureUncertainty (lcRloO7sekK2UgRzAN6): interpretation1_direction: '' has been replaced by 'positive'
temperatureUncertainty (lcRloO7sekK2UgRzAN6): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'
temperatureUncertainty (lcRoeTZpvXUXQDYJbUW): interpretation1_direction: '' has been replaced by 'positive'
temperatureUncertainty (lcRoeTZpvXUXQDYJbUW): interpretation1_seasonalityGeneral: '' has been replaced by 'summer+'
temperature (lcRqPq0E2ipc9svss1o): interpretation1_direction: '' has been replaced by 'positive'
temperature (lcRqPq0E2ipc9svss1o): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'
precipitationUncertainty (lcRt2tvSndxaHJf95q1): interpretation1_variableDetail: 'precip@surface' has been replaced by 'precipitation@surface'
precipitationUncertainty (lcRt2tvSndxaHJf95q1): interpretation1_direction: '' has been replaced by 'positive'
precipitationUncertainty (lcRt2tvSndxaHJf95q1): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'
temperature (lcRut4aNuph5mDCCvOM): interpretation1_direction: '' has been replaced by 'positive'
temperature (lcRut4aNuph5mDCCvOM): interpretation1_seasonalityGeneral: '' has been replaced by 'summer+'
temperature (lcRXwlNyww6riv4ygrW): interpretation1_direction: '' has been replaced by 'positive'
temperature (lcRXwlNyww6riv4ygrW): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'
temperatureUncertainty (lcRxyCa4XQKzGKkEceF): interpretation1_direction: '' has been replaced by 'positive'
temperatureUncertainty (lcRxyCa4XQKzGKkEceF): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'
temperatureUncertainty (lcRyZkdjY6gA9pvlIdZ): interpretation1_direction: '' has been replaced by 'positive'
temperatureUncertainty (lcRyZkdjY6gA9pvlIdZ): interpretation1_seasonalityGeneral: '' has been replaced by 'summer+'
precipitationUncertainty (lcRz8WFv2GH7NS4KdOU): interpretation1_variableDetail: 'precip@surface' has been replaced by 'precipitation@surface'
precipitationUncertainty (lcRz8WFv2GH7NS4KdOU): interpretation1_direction: '' has been replaced by 'positive'
precipitationUncertainty (lcRz8WFv2GH7NS4KdOU): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'
Ravindra, R., 2009. A high-resolution vegetation, fire, and climate history from the Aishihik Region, Yukon Territory, Canada. Master's thesis. University of Ottawa, Ottawa, Ontario, Canada.
A high-resolution vegetation, fire, and climate history from the Aishihik Region, Yukon Territory, Canada.