Harold Lovell

Biographic Data

ID3818034
NAMEHarold Lovell
GIVEN NAMESHarold
FAMILY NAMELovell
SIGNATURELOVELL H
AFFILIATIONSUniversity of Portsmouth
ORCID0000-0002-9435-3178
VERIFIEDYes
TOTAL WORKS8
TOTAL CITATIONS0
AUTHOR COUNT8
EDITOR COUNT0
FIRST PUBLICATION YEAR2011
LATEST PUBLICATION YEAR2024
H-INDEX0

  • Exploring Long-term Landscape Changes in a Rural Catchment in Southern England, from the Mid-nineteenth Century to the Present, and Their Implications for Future Land Management

    Open AccessCat Hudson, Harold Lovell et al.ARTICLELandscapes2024

    Landscapes are shaped by long-term environmental and cultural interactions. The English farming economy has developed in line with shifting land tenure, market integration, and environmental challenges, to its present focus on delivering agri-environmental goods and services under public subsidy. Agricultural intensification, land conversion and enclosure have coalesced into the landscapes observable today. Mid-19th century tithe survey maps offe…

  • Terrestrial glacial geomorphology of surge-type and non-surge-type glaciers on Svalbard

    Open AccessRebecca McCerery, Bethan J Davies et al.ARTICLEJournal of Maps2024

    This paper presents a map of terrestrial glacial geomorphology of eleven surge-type and non-surge-type glacier forefields in southwest and west Spitsbergen, Svalbard. Glacier forefields were mapped using a combination of field surveys and the use of an uncrewed airborne vehicle in September 2022 and satellite imagery captured in 2020, with mapping performed in ArcGIS Pro at a 1:5000 scale. Maps were constructed for glaciers in Van Kuelenfjorden a…

  • Glacial geomorphology in the Wicklow Mountains, Ireland

    Open AccessLauren Knight, Clare M Boston et al.ARTICLEJournal of Maps2023

    We present a detailed 1:50,000-scale glacial geomorphological map covering ∼450 km2 of the Wicklow Mountains, eastern Ireland. The region was glaciated at the Last Glacial Maximum, but little is known about the timing and pattern of deglaciation during the Last Glacial-Interglacial Transition or the extent of glacier regrowth during the Younger Dryas. The absence of detailed glacial geomorphological mapping has been a barrier to understanding the…

  • Evolution of the Norwegian plateau icefield Hardangerjøkulen since the ‘Little Ice Age’

    Open AccessP Weber, Clare M Boston et al.ARTICLEThe Holocene2019References: 5

    The maximum ‘Little Ice Age’ (LIA) glacier extent provides a significant baseline to assess long-term glacier change and to place currently observed rates of glacier recession in a broader temporal context. To that end, we examine the evolution of the plateau icefield Hardangerjøkulen since the LIA. First, we reconstruct Hardangerjøkulen’s maximum LIA extent (~AD 1750) and subsequent recession based on the glacial landform record and aided by his…

  • Manual mapping of drumlins in synthetic landscapes to assess operator effectiveness

    Open AccessJohn K Hillier, M J Smith et al.ARTICLEJournal of Maps2015

    Mapped topographic features are important for understanding processes that sculpt the Earth's surface. This paper presents maps that are the primary product of an exercise that brought together 27 researchers with an interest in landform mapping wherein the efficacy and causes of variation in mapping were tested using novel synthetic DEMs containing drumlins. The variation between interpreters (e.g. mapping philosophy, experience) and across the …

  • A glacial geomorphological map of the southernmost ice lobes of Patagonia

    Open AccessChristopher M Darvill, Chris R Stokes et al.ARTICLEJournal of Maps2014

    This paper presents a glacial geomorphological map of the landforms created by five large ice lobes that extended eastwards from the southernmost reaches of the Patagonian Ice Sheet during the Quaternary period. The study is focussed on Tierra del Fuego, but also updates previous mapping of the Skyring and Otway lobes, and the resulting level of detail and extent is a significant advance on previous work in the region. The map has been created as…

  • Evidence for ice streaming and abrupt high-magnitude proglacial lake drainage in the Seno Skyring-Seno Otway-Strait of Magellan region, southernmost Patagonia

    Open AccessHarold LovellARTICLEQuaternary International2012

  • A glacial geomorphological map of the Seno Skyring-Seno Otway-Strait of Magellan region, southernmost Patagonia

    Open AccessHarold Lovell, Chris R Stokes et al.ARTICLEJournal of Maps2011

    This paper presents a detailed glacial geomorphological map covering over 16,000 km of the Seno Skyring-Seno Otway-Strait of Magellan region in southernmost Patagonia. It builds on previously published maps produced at a variety of scales and is re-mapped in detail for the purposes of reconstructing the pre-Last Glacial Maximum (LGM) glacial dynamics of the region, with particular focus on deciphering the glacial landsystem north east of Seno Otw…