{"help":"Return the metadata of a dataset (package) and its resources. :param id: the id or name of the dataset :type id: string","success":true,"result":[{"id":"e3b0ec3d-2997-4431-8e85-bd8dc6512946","name":"kernel-densities-insect-related-vegetation-damage-2000-2014","title":"Kernel Densities of Insect-related Vegetation Damage from 2000 to 2014","author":"Alaska Center for Conservation Science","maintainer":"Alaska Conservation Science Catalog","maintainer_email":"twnawrocki@alaska.edu","license_title":"https:\/\/creativecommons.org\/licenses\/by-sa\/4.0\/","notes":"\u003Cp\u003EThe four host\/damage type combinations that have contributed the largest areas of forest damage within the study area were correlated to their causal agent(s). Area of forest damage was calculated and described for each of the four most prevalent host\/damage type combinations at five year intervals from 2000 to 2014. Severity of damage for the entire 15-year period from 2000 to 2014 was summarized for insect agents that had associated severity data.\u003C\/p\u003E\n\u003Ch3\u003EKernel Density of Willow Defoliation Caused by Willow Leafblotch Miner\u003C\/h3\u003E\n\u003Cp\u003EFrom 1991 to 1993, willow leafblotch miner defoliated large areas of willow along the Yukon and Kuskokwim Rivers. From 1998 to 1999, a regional willow leafblotch miner outbreak occurred around the Yukon Flats National Wildlife Refuge. Defoliation has occurred on numerous tall and low shrub willow species with the notable exception of felt-leaf willow, which is protected by dense hairs on lower leaf surfaces. The defoliation of willow caused by willow leafblotch miner accounted for over 20% of observed forest damage by area from 2000 to 2014. The area of observed willow defoliation doubled every 5-year period from 2000 to 2014. From 2010 to 2014, approximately 40% of observed forest damage was caused by willow leafblotch miner. This may indicate that environmental conditions are becoming more favorable for willow leafblotch miner within the study area. Most of the defoliation caused by willow leafblotch miner in Alaska occurred within the study area, although more sporadic, widely separated defoliation sites occurred throughout the state.  Kernel Density Estimation was performed using Geospatial Modeling Environment (GME) with points of aspen defoliation damage from 2000 to 2014. The raw kernel density output was interpolated as 5% quantiles of the kernel density values extracted to the original input points. This dataset provides a visualization of area and intensity of impact of aspen leafminer within Alaska from 2000 to 2014.\u003C\/p\u003E\n\u003Cp\u003E\u003Ca href=\u0022\/sites\/default\/files\/styles\/panopoly_image_original\/public\/Figure_WillowLeafblotchMinerDamage.jpg\u0022\u003E\u003Ccenter\u003E\u003Cimg alt=\u0022Kernel density of willow leafblotch miner damage\u0022 title=\u0022Kernel density of willow leafblotch miner damage\u0022 width=\u0022600\u0022 src=\u0022\/sites\/default\/files\/styles\/panopoly_image_original\/public\/Figure_WillowLeafblotchMinerDamage.jpg\u0022 \/\u003E\u003C\/center\u003E\u003C\/a\u003E\u003C\/p\u003E\n\u003Ch3\u003EKernel Density of Damage Caused by Spruce Budworm\u003C\/h3\u003E\n\u003Cp\u003ESpruce defoliation caused by spruce budworm accounted for 6% of observed forest damage by area from 2000 to 2014. However, most of the observed spruce defoliation (around 85%) was low severity (less than half of spruce within damage polygon were defoliated). Spruce budworm did not cause large areas of forest damage from 2010 to 2014: spruce defoliation was relatively high from 2000 to 2004 and 2005 to 2009, and then dropped to almost undetected levels from 2010 to 2014. Spruce budworm outbreaks from 2000 to 2014 were concentrated in areas along the Tanana River near Fairbanks and around the confluence of the Porcupine and Yukon rivers. An additional small aggregation of spruce budworm damage was located on the Kobuk River. Only sporadic, widely separated outbreaks occurred outside these areas. Kernel Density Estimation was performed using Geospatial Modeling Environment (GME) with points of spruce defoliation damage from 2000 to 2014. The raw kernel density output was interpolated as 5% quantiles of the kernel density values extracted to the original input points. This dataset provides a visualization of area and intensity of impact of spruce budworm within Alaska from 2000 to 2014.\u003C\/p\u003E\n\u003Cp\u003E\u003Ca href=\u0022\/sites\/default\/files\/styles\/panopoly_image_original\/public\/Figure_SpruceBudwormDamage.jpg\u0022\u003E\u003Ccenter\u003E\u003Cimg alt=\u0022Kernel density of spruce budworm damage\u0022 title=\u0022Kernel density of spruce budworm damage\u0022 width=\u0022600\u0022 src=\u0022\/sites\/default\/files\/styles\/panopoly_image_original\/public\/Figure_SpruceBudwormDamage.jpg\u0022 \/\u003E\u003C\/center\u003E\u003C\/a\u003E\u003C\/p\u003E\n\u003Ch3\u003EKernel Density of Spruce Mortality Caused by Spruce Beetle\u003C\/h3\u003E\n\u003Cp\u003EWhite spruce has been the most susceptible tree or shrub to mortality from insect and disease agents within the study area. Severity of damage has not been consistently identified for spruce mortality. While spruce beetle outbreaks have caused severe, regional spruce mortality in Southcentral Alaska, spruce beetles have caused only localized and sporadic damage in Interior Alaska. From 2000 to 2014, relatively little spruce beetle damage occurred within the study area. A small region of the 90% isopleth existed along the Yukon River upstream from the confluence with the Porcupine River. However, none of the 80% to 10% isopleths included any area within the study area, and spruce beetle activity was limited north of the eastern and central Alaska Range. From 1990 to 2014, spruce beetle caused only 370 sq km of spruce mortality. This long-term trend suggests that environmental conditions in the study area have historically prevented severe, regional spruce beetle outbreaks. Despite outbreaks being uncommon in the study area, spruce beetles are present in stressed or dying spruce throughout Interior Alaska. Spruce mortality caused by both spruce beetle and northern spruce engraver beetle remained the dominant form of mortality from 2010 to 2014. Kernel Density Estimation was performed using Geospatial Modeling Environment (GME) with points of spruce beetle damage from 2000 to 2014. The raw kernel density output was interpolated as 5% quantiles of the kernel density values extracted to the original input points. This dataset provides a visualization of area and intensity of impact of spruce beetle within Alaska from 2000 to 2014.\u003C\/p\u003E\n\u003Cp\u003E\u003Ca href=\u0022\/sites\/default\/files\/styles\/panopoly_image_original\/public\/Figure_SpruceBeetleDamage.jpg\u0022\u003E\u003Ccenter\u003E\u003Cimg alt=\u0022Kernel density of spruce beetle damage\u0022 title=\u0022Kernel density of spruce beetle damage\u0022 width=\u0022600\u0022 src=\u0022\/sites\/default\/files\/styles\/panopoly_image_original\/public\/Figure_SpruceBeetleDamage.jpg\u0022 \/\u003E\u003C\/center\u003E\u003C\/a\u003E\u003C\/p\u003E\n\u003Ch3\u003EKernel Density of Spruce Mortality Caused by Northern Spruce Engraver Beetle\u003C\/h3\u003E\n\u003Cp\u003EWhite spruce has been the most susceptible tree or shrub to mortality from insect and disease agents within the study area, but the severity of its damage has not been consistently identified. Northern spruce engraver beetle caused approximately 5 times more observed damage by area than spruce beetle. Much of the spruce mortality caused by northern spruce engraver beetle in Alaska fell within the study area, with a high density of the damage occurring north of the confluence of the Porcupine and Yukon Rivers. Northern spruce engraver beetle damage occurred along the lower Noatak River and sporadically throughout the length of the Kobuk River. Spruce mortality caused by both spruce beetle and northern spruce engraver beetle remained the dominant form of mortality from 2010 to 2014, with the northern spruce engraver beetle continuing to contribute more mortality than spruce beetle during those 4 years. The area of spruce mortality caused by northern spruce engraver beetle increased by more than five times between 2000 to 2004 and 2005 to 2009. During 2010 to 2014, activity of northern spruce engraver beetle declined from the amount observed from 2005 to 2009, though not to the levels of 2000 to 2004. Kernel Density Estimation was performed using Geospatial Modeling Environment (GME) with points of spruce damage from 2000 to 2014. The raw kernel density output was interpolated as 5% quantiles of the kernel density values extracted to the original input points. This dataset provides a visualization of area and intensity of impact of northern spruce engraver beetle within Alaska from 2000 to 2014.\u003C\/p\u003E\n\u003Cp\u003E\u003Ca href=\u0022\/sites\/default\/files\/styles\/panopoly_image_original\/public\/Figure_NorthernSpruceEngraverBeetleDamage.jpg\u0022\u003E\u003Ccenter\u003E\u003Cimg alt=\u0022Kernel density of northern spruce engraver beetle damage\u0022 title=\u0022Kernel density of northern spruce engraver beetle damage\u0022 width=\u0022600\u0022 src=\u0022\/sites\/default\/files\/styles\/panopoly_image_original\/public\/Figure_NorthernSpruceEngraverBeetleDamage.jpg\u0022 \/\u003E\u003C\/center\u003E\u003C\/a\u003E\u003C\/p\u003E\n\u003Ch3\u003EKernel Density of Aspen Defoliation Caused by Aspen Leaf Miner\u003C\/h3\u003E\n\u003Cp\u003EThe defoliation of quaking aspen (Populus tremuloides) caused by aspen leaf miner (Phyllocnistis populiella) accounted for over 60% of observed forest damage by area from 2000 to 2014 within the study area. Approximately 40% of aspen defoliation by area was high severity (over half of aspen within the damage polygon were defoliated). From 2010 to 2014, quaking aspen defoliation remained one of the major forms of insect- and disease-related forest damage and accounted for approximately 45% of observed forest damage by area. The area of quaking aspen defoliation has fluctuated every 5-year period between 2000 and 2014 (i.e. 2000 to 2004, 2005 to 2009, and 2010 to 2014) but has always remained the most common form of insect- and disease-related forest damage by area within the study area. The consistently high area of quaking aspen defoliation suggests that environmental conditions steadily favor high populations and\/or frequent outbreaks of aspen leaf miner. Temperature and precipitation have, among other environmental factors, driven the distribution of aspen leaf miner in Alaska. Most aspen defoliation caused by aspen leaf miner in Alaska from 2000 to 2014 occurred within the study area. Kernel Density Estimation was performed using Geospatial Modeling Environment (GME) with points of aspen defoliation damage from 2000 to 2014. The raw kernel density output was interpolated as 5% quantiles of the kernel density values extracted to the original input points. This dataset provides a visualization of area and intensity of impact of aspen leafminer within Alaska from 2000 to 2014.\u003C\/p\u003E\n\u003Cp\u003E\u003Ca href=\u0022\/sites\/default\/files\/styles\/panopoly_image_original\/public\/Figure_AspenLeafminerDamage.jpg\u0022\u003E\u003Ccenter\u003E\u003Cimg alt=\u0022Kernel density of aspen leafminer damage\u0022 title=\u0022Kernel density of aspen leafminer damage\u0022 width=\u0022600\u0022 src=\u0022\/sites\/default\/files\/styles\/panopoly_image_original\/public\/Figure_AspenLeafminerDamage.jpg\u0022 \/\u003E\u003C\/center\u003E\u003C\/a\u003E\u003C\/p\u003E\n","url":"https:\/\/accscatalog.uaa.alaska.edu\/dataset\/kernel-densities-insect-related-vegetation-damage-2000-2014","state":"Active","private":true,"revision_timestamp":"Fri, 10\/03\/2025 - 14:09","metadata_created":"Fri, 02\/23\/2018 - 16:19","metadata_modified":"Fri, 10\/03\/2025 - 14:09","creator_user_id":"d81d7a64-7e59-4e25-83b9-978a7a7aab2c","type":"Dataset","resources":[{"id":"42b9108b-f34c-47d3-966a-a14b52d0ceec","revision_id":"","url":"https:\/\/accscatalog.uaa.alaska.edu\/sites\/default\/files\/REA_CentralYukon_InsectDamage.zip","description":"\u003Cp\u003EThe four host\/damage type combinations that have contributed the largest areas of forest damage within the study area were correlated to their causal agent(s). Area of forest damage was calculated and described for each of the four most prevalent host\/damage type combinations at five year intervals from 2000 to 2014. Severity of damage for the entire 15-year period from 2000 to 2014 was summarized for insect agents that had associated severity data.\u003C\/p\u003E\n\u003Ch3\u003EKernel Density of Willow Defoliation Caused by Willow Leafblotch Miner\u003C\/h3\u003E\n\u003Cp\u003EFrom 1991 to 1993, willow leafblotch miner defoliated large areas of willow along the Yukon and Kuskokwim Rivers. From 1998 to 1999, a regional willow leafblotch miner outbreak occurred around the Yukon Flats National Wildlife Refuge. Defoliation has occurred on numerous tall and low shrub willow species with the notable exception of felt-leaf willow, which is protected by dense hairs on lower leaf surfaces. The defoliation of willow caused by willow leafblotch miner accounted for over 20% of observed forest damage by area from 2000 to 2014. The area of observed willow defoliation doubled every 5-year period from 2000 to 2014. From 2010 to 2014, approximately 40% of observed forest damage was caused by willow leafblotch miner. This may indicate that environmental conditions are becoming more favorable for willow leafblotch miner within the study area. Most of the defoliation caused by willow leafblotch miner in Alaska occurred within the study area, although more sporadic, widely separated defoliation sites occurred throughout the state.  Kernel Density Estimation was performed using Geospatial Modeling Environment (GME) with points of aspen defoliation damage from 2000 to 2014. The raw kernel density output was interpolated as 5% quantiles of the kernel density values extracted to the original input points. This dataset provides a visualization of area and intensity of impact of aspen leafminer within Alaska from 2000 to 2014.\u003C\/p\u003E\n\u003Cp\u003E\u003Ca href=\u0022\/sites\/default\/files\/styles\/panopoly_image_original\/public\/Figure_WillowLeafblotchMinerDamage.jpg\u0022\u003E\u003Ccenter\u003E\u003Cimg alt=\u0022Kernel density of willow leafblotch miner damage\u0022 title=\u0022Kernel density of willow leafblotch miner damage\u0022 width=\u0022600\u0022 src=\u0022\/sites\/default\/files\/styles\/panopoly_image_original\/public\/Figure_WillowLeafblotchMinerDamage.jpg\u0022 \/\u003E\u003C\/center\u003E\u003C\/a\u003E\u003C\/p\u003E\n\u003Ch3\u003EKernel Density of Damage Caused by Spruce Budworm\u003C\/h3\u003E\n\u003Cp\u003ESpruce defoliation caused by spruce budworm accounted for 6% of observed forest damage by area from 2000 to 2014. However, most of the observed spruce defoliation (around 85%) was low severity (less than half of spruce within damage polygon were defoliated). Spruce budworm did not cause large areas of forest damage from 2010 to 2014: spruce defoliation was relatively high from 2000 to 2004 and 2005 to 2009, and then dropped to almost undetected levels from 2010 to 2014. Spruce budworm outbreaks from 2000 to 2014 were concentrated in areas along the Tanana River near Fairbanks and around the confluence of the Porcupine and Yukon rivers. An additional small aggregation of spruce budworm damage was located on the Kobuk River. Only sporadic, widely separated outbreaks occurred outside these areas. Kernel Density Estimation was performed using Geospatial Modeling Environment (GME) with points of spruce defoliation damage from 2000 to 2014. The raw kernel density output was interpolated as 5% quantiles of the kernel density values extracted to the original input points. This dataset provides a visualization of area and intensity of impact of spruce budworm within Alaska from 2000 to 2014.\u003C\/p\u003E\n\u003Cp\u003E\u003Ca href=\u0022\/sites\/default\/files\/styles\/panopoly_image_original\/public\/Figure_SpruceBudwormDamage.jpg\u0022\u003E\u003Ccenter\u003E\u003Cimg alt=\u0022Kernel density of spruce budworm damage\u0022 title=\u0022Kernel density of spruce budworm damage\u0022 width=\u0022600\u0022 src=\u0022\/sites\/default\/files\/styles\/panopoly_image_original\/public\/Figure_SpruceBudwormDamage.jpg\u0022 \/\u003E\u003C\/center\u003E\u003C\/a\u003E\u003C\/p\u003E\n\u003Ch3\u003EKernel Density of Spruce Mortality Caused by Spruce Beetle\u003C\/h3\u003E\n\u003Cp\u003EWhite spruce has been the most susceptible tree or shrub to mortality from insect and disease agents within the study area. Severity of damage has not been consistently identified for spruce mortality. While spruce beetle outbreaks have caused severe, regional spruce mortality in Southcentral Alaska, spruce beetles have caused only localized and sporadic damage in Interior Alaska. From 2000 to 2014, relatively little spruce beetle damage occurred within the study area. A small region of the 90% isopleth existed along the Yukon River upstream from the confluence with the Porcupine River. However, none of the 80% to 10% isopleths included any area within the study area, and spruce beetle activity was limited north of the eastern and central Alaska Range. From 1990 to 2014, spruce beetle caused only 370 sq km of spruce mortality. This long-term trend suggests that environmental conditions in the study area have historically prevented severe, regional spruce beetle outbreaks. Despite outbreaks being uncommon in the study area, spruce beetles are present in stressed or dying spruce throughout Interior Alaska. Spruce mortality caused by both spruce beetle and northern spruce engraver beetle remained the dominant form of mortality from 2010 to 2014. Kernel Density Estimation was performed using Geospatial Modeling Environment (GME) with points of spruce beetle damage from 2000 to 2014. The raw kernel density output was interpolated as 5% quantiles of the kernel density values extracted to the original input points. This dataset provides a visualization of area and intensity of impact of spruce beetle within Alaska from 2000 to 2014.\u003C\/p\u003E\n\u003Cp\u003E\u003Ca href=\u0022\/sites\/default\/files\/styles\/panopoly_image_original\/public\/Figure_SpruceBeetleDamage.jpg\u0022\u003E\u003Ccenter\u003E\u003Cimg alt=\u0022Kernel density of spruce beetle damage\u0022 title=\u0022Kernel density of spruce beetle damage\u0022 width=\u0022600\u0022 src=\u0022\/sites\/default\/files\/styles\/panopoly_image_original\/public\/Figure_SpruceBeetleDamage.jpg\u0022 \/\u003E\u003C\/center\u003E\u003C\/a\u003E\u003C\/p\u003E\n\u003Ch3\u003EKernel Density of Spruce Mortality Caused by Northern Spruce Engraver Beetle\u003C\/h3\u003E\n\u003Cp\u003EWhite spruce has been the most susceptible tree or shrub to mortality from insect and disease agents within the study area, but the severity of its damage has not been consistently identified. Northern spruce engraver beetle caused approximately 5 times more observed damage by area than spruce beetle. Much of the spruce mortality caused by northern spruce engraver beetle in Alaska fell within the study area, with a high density of the damage occurring north of the confluence of the Porcupine and Yukon Rivers. Northern spruce engraver beetle damage occurred along the lower Noatak River and sporadically throughout the length of the Kobuk River. Spruce mortality caused by both spruce beetle and northern spruce engraver beetle remained the dominant form of mortality from 2010 to 2014, with the northern spruce engraver beetle continuing to contribute more mortality than spruce beetle during those 4 years. The area of spruce mortality caused by northern spruce engraver beetle increased by more than five times between 2000 to 2004 and 2005 to 2009. During 2010 to 2014, activity of northern spruce engraver beetle declined from the amount observed from 2005 to 2009, though not to the levels of 2000 to 2004. Kernel Density Estimation was performed using Geospatial Modeling Environment (GME) with points of spruce damage from 2000 to 2014. The raw kernel density output was interpolated as 5% quantiles of the kernel density values extracted to the original input points. This dataset provides a visualization of area and intensity of impact of northern spruce engraver beetle within Alaska from 2000 to 2014.\u003C\/p\u003E\n\u003Cp\u003E\u003Ca href=\u0022\/sites\/default\/files\/styles\/panopoly_image_original\/public\/Figure_NorthernSpruceEngraverBeetleDamage.jpg\u0022\u003E\u003Ccenter\u003E\u003Cimg alt=\u0022Kernel density of northern spruce engraver beetle damage\u0022 title=\u0022Kernel density of northern spruce engraver beetle damage\u0022 width=\u0022600\u0022 src=\u0022\/sites\/default\/files\/styles\/panopoly_image_original\/public\/Figure_NorthernSpruceEngraverBeetleDamage.jpg\u0022 \/\u003E\u003C\/center\u003E\u003C\/a\u003E\u003C\/p\u003E\n\u003Ch3\u003EKernel Density of Aspen Defoliation Caused by Aspen Leaf Miner\u003C\/h3\u003E\n\u003Cp\u003EThe defoliation of quaking aspen (Populus tremuloides) caused by aspen leaf miner (Phyllocnistis populiella) accounted for over 60% of observed forest damage by area from 2000 to 2014 within the study area. Approximately 40% of aspen defoliation by area was high severity (over half of aspen within the damage polygon were defoliated). From 2010 to 2014, quaking aspen defoliation remained one of the major forms of insect- and disease-related forest damage and accounted for approximately 45% of observed forest damage by area. The area of quaking aspen defoliation has fluctuated every 5-year period between 2000 and 2014 (i.e. 2000 to 2004, 2005 to 2009, and 2010 to 2014) but has always remained the most common form of insect- and disease-related forest damage by area within the study area. The consistently high area of quaking aspen defoliation suggests that environmental conditions steadily favor high populations and\/or frequent outbreaks of aspen leaf miner. Temperature and precipitation have, among other environmental factors, driven the distribution of aspen leaf miner in Alaska. Most aspen defoliation caused by aspen leaf miner in Alaska from 2000 to 2014 occurred within the study area. Kernel Density Estimation was performed using Geospatial Modeling Environment (GME) with points of aspen defoliation damage from 2000 to 2014. The raw kernel density output was interpolated as 5% quantiles of the kernel density values extracted to the original input points. This dataset provides a visualization of area and intensity of impact of aspen leafminer within Alaska from 2000 to 2014.\u003C\/p\u003E\n\u003Cp\u003E\u003Ca href=\u0022\/sites\/default\/files\/styles\/panopoly_image_original\/public\/Figure_AspenLeafminerDamage.jpg\u0022\u003E\u003Ccenter\u003E\u003Cimg alt=\u0022Kernel density of aspen leafminer damage\u0022 title=\u0022Kernel density of aspen leafminer damage\u0022 width=\u0022600\u0022 src=\u0022\/sites\/default\/files\/styles\/panopoly_image_original\/public\/Figure_AspenLeafminerDamage.jpg\u0022 \/\u003E\u003C\/center\u003E\u003C\/a\u003E\u003C\/p\u003E\n","format":"zip","state":"Active","revision_timestamp":"Fri, 02\/01\/2019 - 11:16","name":"Kernel Densities of Insect-related Forest Damage from 2000 to 2014","mimetype":"application\/zip","size":"817.32 KB","created":"Fri, 02\/23\/2018 - 16:20","resource_group_id":"","last_modified":"Date changed  Fri, 02\/01\/2019 - 11:16"},{"id":"7ad1d20a-efc6-4443-9f41-822c6a02b95a","revision_id":"","url":"https:\/\/accscatalog.uaa.alaska.edu\/sites\/default\/files\/REA_CentralYukon_Report.pdf","description":"\u003Cp\u003EThe assessment area, referred to in this REA as the Central Yukon (CYR) study area, includes a core of seven ecoregions selected by BLM: Brooks Range (south of the ridge crest), Davidson Mountains, Kobuk Ridges and Valleys, North Ogilvie Mountains, Ray Mountains, Yukon\u2013Old Crow Basin, and Yukon-Tanana Uplands. Ecoregions in this assessment were defined by Nowacki et al. (2001) and represent a unified mapping approach that blends traditional approaches with regionally-specific knowledge and ecological goals. Following BLM guidelines, the study area was formed by buffering the selected ecoregions by any 5th-level hydrologic units that intersected the ecoregion boundaries. Additionally, at the request of the BLM, the assessment boundary includes key lands surrounding the Dalton Highway on the north edge of the study area. Most of the Kotzebue Sound Lowlands are included in the study area because of the buffer region. The buffer region additionally causes the inclusion of small portions of several ecoregions along the southern boundary of the study area: these portions have been modified into a conglomerate unique to this REA referred to as the Tanana-Kuskokwim-Yukon Lowlands.\u003C\/p\u003E\n\u003Cp\u003EThis region has a boreal climate, with long cold winters and relatively brief but warm summers. Climate varies depending primarily upon elevation, proximity to the coast, and latitude. Although in general the most extreme cold occurs at high elevations, some areas experience localized temperature inversions. With mean annual temperatures below freezing in most areas, but above freezing in others, permafrost is discontinuous. This discontinuity occurs at both fine scales and broader scales.\u003C\/p\u003E\n\u003Cp\u003EThe Final Report contains the detailed results from the Central Yukon Rapid Ecoregional Assessment. The Central Yukon REA does not include a Manager\u0027s Summary document.\u003C\/p\u003E\n","format":"pdf","state":"Active","revision_timestamp":"Thu, 02\/07\/2019 - 20:45","name":"Central Yukon REA Final Report","mimetype":"application\/pdf","size":"76.95 MB","created":"Fri, 02\/23\/2018 - 14:06","resource_group_id":"","last_modified":"Date changed  Thu, 02\/07\/2019 - 20:45"}],"tags":[{"id":"880c41cc-62aa-4ace-bb50-4b95fc21dbd2","vocabulary_id":"2","name":"insects"},{"id":"8cbf8a5a-c2b2-476e-bb0c-759b4fb94173","vocabulary_id":"2","name":"boreal"},{"id":"9bd42380-a90d-411d-974c-76a1c75ad1ca","vocabulary_id":"2","name":"vegetation"}]}]}