Sally Thompson
Biographic Data
| ID | 5845955 |
|---|---|
| NAME | Sally Thompson |
| GIVEN NAMES | Sally |
| FAMILY NAME | Thompson |
| SIGNATURE | THOMPSON S |
| AFFILIATIONS | Monash University |
| ORCID | 0000-0003-0534-9394 |
| VERIFIED | Yes |
| TOTAL WORKS | 8 |
| TOTAL CITATIONS | 0 |
| AUTHOR COUNT | 8 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2017 |
| LATEST PUBLICATION YEAR | 2026 |
| H-INDEX | 0 |
Literacy mediation
Automated property parcel classification using very high-resolution land cover imagery and multi-modal deep learning
This study addresses the challenges of monitoring urban development where sprawl, infill and soft densification are prevalent. To accurately identify the spatial distribution and characteristics of different development types, a multi-modal deep learning model was developed to predict parcel-level development types using very high-resolution land cover maps and tabular data representing parcel attributes of surface cover, built form and dwelling …
Subsurface constraints amplify vegetation stress during extreme heat and drought in a Mediterranean forest
Drought and extreme heat events are becoming more frequent and intense as the global climate warms, threatening forests worldwide. Subsurface conditions such as soil depth and groundwater availability can influence plant drought vulnerability. Yet, how subsurface factors interact with climate stress and shape forest vulnerability and die-off at landscape scales remains poorly understood. The record-breaking hot and dry 2023–2024 summer in southwe…
Biophysical response of a coastal woodland to extreme water deficit during a year of record-breaking heat
Global terrestrial and ocean surface temperatures continue to reach record levels, resulting in heat waves, drought, and prolonged heat stress experienced by vegetation in many regions. In 2023–2024, coastal terrestrial ecosystems in Western Australia were particularly affected, experiencing their driest and hottest summer since observations began in the early 1900s. Banksia woodlands are a threatened ecological community in this region that are …
Deforestation-induced surface warming is influenced by the fragmentation and spatial extent of forest loss in Maritime Southeast Asia
Deforestation in the tropics causes warming which contributes to regional climate change. Forest loss occurs over a broad range of spatial scales, producing a variety of spatial patterns of cleared and forested land. Whether the spatial attributes of these patterns influence the resulting temperature change remains largely unknown. We adopted a differences-in-differences approach to analyse remotely-sensed forest loss and land surface temperature…
Plants as sensors
In Mediterranean-type climates, asynchronicity between energy and water availability means that ecosystems rely heavily on the water-storing capacity of the subsurface to sustain plant water use over the summer dry season. The root-zone water storage capacity ( S m a x [L]) defines the maximum volume of water that can be stored in plant accessible locations in the subsurface, but is poorly characterized and difficult to measure at large scales. H…
Forest loss in Brazil increases maximum temperatures within 50 km
Forest cover loss in the tropics is well known to cause warming at deforested sites, with maximum temperatures being particularly sensitive. Forest loss causes warming by altering local energy balance and surface roughness, local changes that can propagate across a wide range of spatial scales. Consequently, temperature increases result from not only changes in forest cover at a site, but also by the aggregate effects of non-local forest loss. We…
How competitive is drought deciduousness in tropical forests? A combined eco-hydrological and eco-evolutionary approach
Drought-deciduous and evergreen species are both common in tropical forests, where there is the need to cope with water shortages during periodic dry spells and over the course of the dry season. Which phenological strategy is favored depends on the long-term balance of carbon costs and gains that leaf phenology imposes as a result of the alternation of wet and dry seasons and the unpredictability of rainfall events. This study integrates a stoch…
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How competitive is drought deciduousness in tropical forests? A combined eco-hydrological and eco-evolutionary approach
Drought-deciduous and evergreen species are both common in tropical forests, where there is the need to cope with water shortages during periodic dry spells and over the course of the dry season. Which phenological strategy is favored depends on the long-term balance of carbon costs and gains that leaf phenology imposes as a result of the alternation of wet and dry seasons and the unpredictability of rainfall events. This study integrates a stoch…
Forest loss in Brazil increases maximum temperatures within 50 km
Forest cover loss in the tropics is well known to cause warming at deforested sites, with maximum temperatures being particularly sensitive. Forest loss causes warming by altering local energy balance and surface roughness, local changes that can propagate across a wide range of spatial scales. Consequently, temperature increases result from not only changes in forest cover at a site, but also by the aggregate effects of non-local forest loss. We…
Plants as sensors
In Mediterranean-type climates, asynchronicity between energy and water availability means that ecosystems rely heavily on the water-storing capacity of the subsurface to sustain plant water use over the summer dry season. The root-zone water storage capacity ( S m a x [L]) defines the maximum volume of water that can be stored in plant accessible locations in the subsurface, but is poorly characterized and difficult to measure at large scales. H…
Deforestation-induced surface warming is influenced by the fragmentation and spatial extent of forest loss in Maritime Southeast Asia
Deforestation in the tropics causes warming which contributes to regional climate change. Forest loss occurs over a broad range of spatial scales, producing a variety of spatial patterns of cleared and forested land. Whether the spatial attributes of these patterns influence the resulting temperature change remains largely unknown. We adopted a differences-in-differences approach to analyse remotely-sensed forest loss and land surface temperature…
Automated property parcel classification using very high-resolution land cover imagery and multi-modal deep learning
This study addresses the challenges of monitoring urban development where sprawl, infill and soft densification are prevalent. To accurately identify the spatial distribution and characteristics of different development types, a multi-modal deep learning model was developed to predict parcel-level development types using very high-resolution land cover maps and tabular data representing parcel attributes of surface cover, built form and dwelling …
Subsurface constraints amplify vegetation stress during extreme heat and drought in a Mediterranean forest
Drought and extreme heat events are becoming more frequent and intense as the global climate warms, threatening forests worldwide. Subsurface conditions such as soil depth and groundwater availability can influence plant drought vulnerability. Yet, how subsurface factors interact with climate stress and shape forest vulnerability and die-off at landscape scales remains poorly understood. The record-breaking hot and dry 2023–2024 summer in southwe…
Biophysical response of a coastal woodland to extreme water deficit during a year of record-breaking heat
Global terrestrial and ocean surface temperatures continue to reach record levels, resulting in heat waves, drought, and prolonged heat stress experienced by vegetation in many regions. In 2023–2024, coastal terrestrial ecosystems in Western Australia were particularly affected, experiencing their driest and hottest summer since observations began in the early 1900s. Banksia woodlands are a threatened ecological community in this region that are …
Literacy mediation
Climate change (5 works) · Ecology (4 works) · Environmental Science (4 works) · Plant Water Relations and Carbon Dynamics (4 works) · Geology (3 works) · Land Use and Ecosystem Services (3 works) · Agroforestry (2 works) · Biology (2 works) · Climate change and permafrost (2 works) · Climatology (2 works)