Mathew Allan

Dr. Mathew Allan

orcid

Research Focus & Metrics

Academic Career Length

16Years (2011-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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17 March 2015 in Scientific Data
Verified
Journal Article
Open access
SSSapna Sharma
Sapna Sharma
DGDerek K Gray
Derek K Gray
JRJordan S Read
Jordan S Read
COCatherine M O’reilly
Catherine M O’reilly
PSPhilipp Schneider
Philipp Schneider
KWKara H Woo
Kara H Woo
Global environmental change has influenced lake surface temperatures, a key driver of ecosystem structure and function. Recent studies have suggested significant warming of water temperatures in individual lakes across many different regions around the world. However, the spatial and temporal coherence associated with the magnitude of these trends remains unclear. Thus, a global data set of water temperature is required to understand and synthesize global, long-term trends in surface water temperatures of inland bodies of water. We assembled a database of summer lake surface temperatures for 291 lakes collected in situ and/or by satellites for the period 1985–2009. In addition, corresponding climatic drivers (air temperatures, solar radiation, and cloud cover) and geomorphometric characteristics (latitude, longitude, elevation, lake surface area, maximum depth, mean depth, and volume) that influence lake surface temperatures were compiled for each lake. This unique dataset offers an invaluable baseline perspective on global-scale lake thermal conditions as environmental change continues.

28 March 2011 in International Journal of Remote Sensing
Verified
Journal Article
Closed access
MAMathew Allan
Mathew Allan
DHDavid Hamilton
David Hamilton
BHBrendan Hicks
Brendan Hicks
LBLars Brabyn
Lars Brabyn
We investigated the use of Landsat Enhanced Thematic Mapper (ETM) imagery to synoptically quantify chlorophyll a (chl a) concentrations. Two adjoining pairs of images of the central North Island were acquired on two different days in summer and spring 2002. 6sv atmospheric correction was compared to the cosine of the solar zenith angle correction (COST) dark object subtraction (DOS) atmospheric correction. The highest correlation between 6sv ln(Band 3) water surface reflectance and ln(chl a) was found in the 24 January 2002 image (r 2 = 0.954). 6sv atmospheric correction was preferable to COST-DOS as it gave more realistic reflectance values at a clear-water reference site and produced the highest correlation coefficient. The results from this investigation suggest that remote sensing provides a valuable tool to assess temporal and spatial distributions of chl a in unmonitored areas within lakes and that predictions may also be extended to unmonitored lakes within the domain of satellite image capture.

10 July 2014 in Journal of Geophysical Research: Biogeosciences
Verified
Journal Article
Open access
PDF file
KRKevin C. Rose
Kevin C. Rose
DHDavid Hamilton
David Hamilton
CWCraig E. Williamson
Craig E. Williamson
CMChris G. McBride
Chris G. McBride
JFJanet M. Fischer
Janet M. Fischer
NCNathalie Cabrol
Nathalie Cabrol
Transparency is a fundamental characteristic of aquatic ecosystems and is highly responsive to changes in climate and land use. The transparency of glacially‐fed lakes may be a particularly sensitive sentinel characteristic of these changes. However, little is known about the relative contributions of glacial flour versus other factors affecting light attenuation in these lakes. We sampled 18 glacially‐fed lakes in Chile, New Zealand, and the U.S. and Canadian Rocky Mountains to characterize how dissolved absorption, algal biomass (approximated by chlorophyll a), water, and glacial flour contributed to attenuation of ultraviolet radiation (UVR) and photosynthetically active radiation (PAR, 400–700 nm). Variation in attenuation across lakes was related to turbidity, which we used as a proxy for the concentration of glacial flour. Turbidity‐specific diffuse attenuation coefficients increased with decreasing wavelength and distance from glaciers. Regional differences in turbidity‐specific diffuse attenuation coefficients were observed in short UVR wavelengths (305 and 320 nm) but not at longer UVR wavelengths (380 nm) or PAR. Dissolved absorption coefficients, which are closely correlated with diffuse attenuation coefficients in most non‐glacially‐fed lakes, represented only about one quarter of diffuse attenuation coefficients in study lakes here, whereas glacial flour contributed about two thirds across UVR and PAR. Understanding the optical characteristics of substances that regulate light attenuation in glacially‐fed lakes will help elucidate the signals that these systems provide of broader environmental changes and forecast the effects of climate change on these aquatic ecosystems.

13 August 2018 in Remote Sensing
Verified
Journal Article
Open access
PDF file
MLMoritz Lehmann
Moritz Lehmann
UNUyen Nguyen
Uyen Nguyen
MAMathew Allan
Mathew Allan
HWHans van der Woerd
Hans van der Woerd
Remote sensing by satellite-borne sensors presents a significant opportunity to enhance the spatio-temporal coverage of environmental monitoring programmes for lakes, but the estimation of classic water quality attributes from inland water bodies has not reached operational status due to the difficulty of discerning the spectral signatures of optically active water constituents. Determination of water colour, as perceived by the human eye, does not require knowledge of inherent optical properties and therefore represents a generally applicable remotely-sensed water quality attribute. In this paper, we implemented a recent algorithm for the retrieval of colour parameters (hue angle, dominant wavelength) and derived a new correction for colour purity to account for the spectral bandpass of the Landsat 8 Operational Land Imager (OLI). We used this algorithm to calculate water colour on almost 45,000 observations over four years from 1486 lakes from a diverse range of optical water types in New Zealand. We show that the most prevalent lake colours are yellow-orange and blue, respectively, while green observations are comparatively rare. About 40% of the study lakes show transitions between colours at a range of time scales, including seasonal. A preliminary exploratory analysis suggests that both geo-physical and anthropogenic factors, such as catchment land use, provide environmental control of lake colour and are promising avenues for future analysis.

1 October 2013 in Ecological Modelling
Verified
Journal Article
Open access
AKA.R. Keshtkar
A.R. Keshtkar
ASA. Salajegheh
A. Salajegheh
ASA. Sadoddin
A. Sadoddin
MAMathew Allan
Mathew Allan
Catchment management is a process which increases the sustainable development and management of all catchment resources in order to maximize the balance among socioeconomic welfare and the sustainability of vital ecosystems. The increase of anthropogenic activities within river catchments causes degradation and serious problems for stakeholders and managers, particularly in arid and semi-arid regions. Although there are many techniques for solving these problems, it is not easy for catchment managers to apply them. An integrated Bayesian network model framework was applied to evaluate the sustainability of a semi-arid river catchment located in the Iranian Central Plateau river basin encompassing 32.6km2 area on the Hablehrood river catchment, located in the northern part of the Iranian Central Plateau river basin. The research illustrated the assessment of the relevant management problems, the model framework, and the techniques applied to extract input data. Results for the study area implementation and a suggestion for management are described and discussed

22 February 2013 in Environmental Monitoring and Assessment
Verified
Journal Article
Closed access
PDF file
BHBrendan Hicks
Brendan Hicks
GSGlen A. Stichbury
Glen A. Stichbury
LBLars Brabyn
Lars Brabyn
MAMathew Allan
Mathew Allan
SASalman Ashraf
Salman Ashraf