Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

Long‐term recovery patterns of arctic tundra after winter seismic exploration

View through CrossRef
In response to the increasing global demand for energy, oil exploration and development are expanding into frontier areas of the Arctic, where slow‐growing tundra vegetation and the underlying permafrost soils are very sensitive to disturbance. The creation of vehicle trails on the tundra from seismic exploration for oil has accelerated in the past decade, and the cumulative impact represents a geographic footprint that covers a greater extent of Alaska's North Slope tundra than all other direct human impacts combined. Seismic exploration for oil and gas was conducted on the coastal plain of the Arctic National Wildlife Refuge, Alaska, USA, in the winters of 1984 and 1985. This study documents recovery of vegetation and permafrost soils over a two‐decade period after vehicle traffic on snow‐covered tundra. Paired permanent vegetation plots (disturbed vs. reference) were monitored six times from 1984 to 2002. Data were collected on percent vegetative cover by plant species and on soil and ground ice characteristics. We developed Bayesian hierarchical models, with temporally and spatially autocorrelated errors, to analyze the effects of vegetation type and initial disturbance levels on recovery patterns of the different plant growth forms as well as soil thaw depth. Plant community composition was altered on the trails by species‐specific responses to initial disturbance and subsequent changes in substrate. Long‐term changes included increased cover of graminoids and decreased cover of evergreen shrubs and mosses. Trails with low levels of initial disturbance usually improved well over time, whereas those with medium to high levels of initial disturbance recovered slowly. Trails on ice‐poor, gravel substrates of riparian areas recovered better than those on ice‐rich loamy soils of the uplands, even after severe initial damage. Recovery to pre‐disturbance communities was not possible where trail subsidence occurred due to thawing of ground ice. Previous studies of disturbance from winter seismic vehicles in the Arctic predicted short‐term and mostly aesthetic impacts, but we found that severe impacts to tundra vegetation persisted for two decades after disturbance under some conditions. We recommend management approaches that should be used to prevent persistent tundra damage.
Title: Long‐term recovery patterns of arctic tundra after winter seismic exploration
Description:
In response to the increasing global demand for energy, oil exploration and development are expanding into frontier areas of the Arctic, where slow‐growing tundra vegetation and the underlying permafrost soils are very sensitive to disturbance.
The creation of vehicle trails on the tundra from seismic exploration for oil has accelerated in the past decade, and the cumulative impact represents a geographic footprint that covers a greater extent of Alaska's North Slope tundra than all other direct human impacts combined.
Seismic exploration for oil and gas was conducted on the coastal plain of the Arctic National Wildlife Refuge, Alaska, USA, in the winters of 1984 and 1985.
This study documents recovery of vegetation and permafrost soils over a two‐decade period after vehicle traffic on snow‐covered tundra.
Paired permanent vegetation plots (disturbed vs.
reference) were monitored six times from 1984 to 2002.
Data were collected on percent vegetative cover by plant species and on soil and ground ice characteristics.
We developed Bayesian hierarchical models, with temporally and spatially autocorrelated errors, to analyze the effects of vegetation type and initial disturbance levels on recovery patterns of the different plant growth forms as well as soil thaw depth.
Plant community composition was altered on the trails by species‐specific responses to initial disturbance and subsequent changes in substrate.
Long‐term changes included increased cover of graminoids and decreased cover of evergreen shrubs and mosses.
Trails with low levels of initial disturbance usually improved well over time, whereas those with medium to high levels of initial disturbance recovered slowly.
Trails on ice‐poor, gravel substrates of riparian areas recovered better than those on ice‐rich loamy soils of the uplands, even after severe initial damage.
Recovery to pre‐disturbance communities was not possible where trail subsidence occurred due to thawing of ground ice.
Previous studies of disturbance from winter seismic vehicles in the Arctic predicted short‐term and mostly aesthetic impacts, but we found that severe impacts to tundra vegetation persisted for two decades after disturbance under some conditions.
We recommend management approaches that should be used to prevent persistent tundra damage.

Related Results

한국의 북극 거버넌스 구축 및 참여 전략 (Changes in the Arctic and Establishment of New Arctic Governance)
한국의 북극 거버넌스 구축 및 참여 전략 (Changes in the Arctic and Establishment of New Arctic Governance)
<b>Korean Abstract:</b> 21세기 들어 북극 지역의 변화가 가시화되면서 북극이 새롭게 조명을 받고 있다. ‘북극의 변화’는 상호 밀접한 관계를 지닌 세 가지 변화가 중심을 이루고 있다. 첫 번째는 기후변화로 인해 북극의 해빙 속도가 보다 빨라지고 그 범위가 점차 확대되면서, 국제사회...
Quantifying Arctic Storm Risk in a Changing Climate
Quantifying Arctic Storm Risk in a Changing Climate
&lt;p&gt;The Arctic has undergone significant change over the past few decades, and there has been great reductions in Arctic sea ice extent. The Arctic ocean has become mo...
Freshwater Carbon Across Arctic Lowland Tundra Ecosystems
Freshwater Carbon Across Arctic Lowland Tundra Ecosystems
Arctic lowland tundra landscapes are low-relief regions located in the high latitudes of the Northern Hemisphere and are underlain by permafrost, a defining feature that regulates ...
Late Quaternary History of Tundra Vegetation in Northwestern Alaska
Late Quaternary History of Tundra Vegetation in Northwestern Alaska
AbstractPollen analysis of a new core from Joe Lake indicates that the late Quaternary vegetation of northwestern Alaska was characterized by four tundra and two forest-tundra type...
Breaking the Ice Barrier
Breaking the Ice Barrier
ABSTRACT Recent seismic data collection in previously unnavigated waters of the Canadian High Arctic (as far north as Kane Basin and west to the western entrance ...
4D Seismic on Gullfaks
4D Seismic on Gullfaks
SUMMARY New technologies are rapidly emerging helping to obtain optimal drainage of large reservoirs. 4D seismic is such a reservoir monitoring technique. The phy...
Seismic Frequency Enhancement for Mapping and Reservoir Characterization of Arab Formation: Case Study Onshore UAE
Seismic Frequency Enhancement for Mapping and Reservoir Characterization of Arab Formation: Case Study Onshore UAE
Abstract Mapping and discrimination of Upper Jurassic Arab reservoirs (Arab A/B/C and D) in this 3D seismic onshore field of Abu Dhabi, is very sensitive to the seis...
The Polar Silk Road and China's role in Arctic governance
The Polar Silk Road and China's role in Arctic governance
The People's Republic of China (PRC) wants to become a key regional actor in the Arctic. PRC's underlying priority in the region is gaining access to commercial opportunities from ...

Back to Top