Abstracts:
CMOS
Ottawa, 2022-2023
(in
language
given)
Wang: Northern peatlands
cover about 4 million km2, and half of these
peatlands are estimated to contain permafrost and periglacial
landforms, such as palsas and peat plateaus. In Labrador, northeastern
Canada, peatland permafrost landforms are largely predicted to be
present in the interior and absent along the coastline. However, few
observations of these landforms in the interior, coupled with extensive
use of coastal perennially frozen peatlands for traditional activities
by Labrador Inuit and Innu suggests a need for further investigations.
In 2020, the Northern Environmental Geoscience Laboratory began a new
research program to better understand the distribution,
characteristics, and sensitivity of peatland permafrost in coastal
Labrador using a combination of research methods including remote
sensing, machine learning, field investigations, and thermal modelling.
The
first stage
of this project involved the development of a consensus-based inventory
of prospective peatland permafrost complexes using high-resolution
satellite imagery. The inventory, which identified over 1000 likely
peatland permafrost complexes within 100 km of the Labrador Sea
coastline, has been validated with extensive field visits and
low-altitude aerial photography and videography. A coastal gradient for
palsa and peat plateau distribution was identified and is thought to be
attributed to a combination of climatic and geomorphological
influences. Other initiatives as part of this overarching project
include historical air photo analysis to identify the scale of thaw at
selected complexes over the past 70 years and characterization of
contemporary peatland permafrost landform heights, sizes, and
associated snow and vegetation conditions at selected complexes along
the coast using remotely piloted aircraft surveys. This work provides
an important baseline for future mapping, modelling, and climate change
adaptation strategy development in northeastern Canada.
Shkvorets: The
world ocean
is the global thermodynamic engine of
weather and climate; without ocean data collection on a global scale,
it is impossible to define problems of climate change.
Modern oceanographic data collection technologies include four thousand
autonomous Argo floats, deployed globally in all oceans. These
profile every 10 days from a depth of 2000m to the surface to collect
temperature, salinity and other physical-chemical data. The rest
of the time the floats drift while parked at a depth of 1000m.
This depth limits the areas of use of Argo floats in coastal waters
where, when reaching shallow water, their mission is usually
terminated. The cohort of Argo floats may be complemented by a flotilla
of small craft. To help fill this gap in oceanographic data, the
author co-founded a non-for-profit project "Sail for Science"
www.sailforscience.com, with the following objectives:
1. To collect low-cost high-quality oceanographic data
using RBR Ltd. (Ottawa, Canada) compact, reliable, easy operating
CTD (Conductivity, Temperature, Depth) systems; and
2. To develop a methodology and best practice recommendations for
citizen scientists on how to use RBR CTD systems to collect data,
provide Quality Control of data, and transfer these data to the
National Oceanographic Data Centres.
The presentation demonstrates how modern measurement technologies make
it possible to expand citizen science to the new level of collecting
high-precision oceanographic data.
Shan: Coastal
upwelling is a prominent oceanic process
that brings nutrient-rich deep waters to the sunlit surface, thereby
regulating many productive fisheries and marine ecosystems around the
globe. How the frequency, intensity, and duration of coastal upwelling
might shift in a warming climate is therefore a question of vital
importance. In the first part of my presentation, I will discuss
the temporal and
spatial characteristics of the major wind-driven summertime coastal
upwelling events off Nova Scotia. In the second part, I will
examine trends in coastal upwelling off Nova Scotia over the past two
decades based on observations made from various platforms, including
marine buoys, remote-sensing satellites, and autonomous underwater
gliders. A series of novel upwelling metrics are derived to describe
coastal
upwelling trends in terms of frequency, intensity, and duration. The
predictability of observed upwelling trends is also explored by
assessing the performance of coastal operational model products.
Ariya:
Particles, nano, micro and
macro-particles, are
ubiquitous on Earth. They are chemically, physically, and biologically
diverse. They are naturally produced or increasingly through numerous
anthropogenic activities, namely medicine-health, chemical industries,
materials, construction, transport, communication, aerospace,
agriculture, and energy sectors. Air pollution, particularly
airborne nano-size particles, have been identified as the cause of
about 6 million premature deaths (WHO, 2020). Aerosols are also
significant in climate change and Earth’s energy processes. They play a
role in radiation, ice nucleation and precipitation events (IPCC,
2018). The identified gap of knowledge by both the IPCC and the WHO are
converging, and it becomes clear that they are related to the
physicochemical characteristics of particles. Air and water are in
motion, as are the particles in air and water. We should be able to
observe, track, characterize and remediate in-situ and real-time in 4D
(3 dimensions and time). In this talk, we provide an overview of the
recent advances in this lab to help to fill the gap identified by the
IPCC and the WHO in the age of climate change and COVID-19. We discuss
the development of novel promising technologies for fast in-situ and
real-time observation of aerosols and waterborne viruses and
physicochemical transformations and ice nucleation of anthropogenic
emerging nanoparticles (e.g., nano-plastics in air/water). We explore
some links between fundamental studies that provide advances in
designing zero-net energy and recyclable technology using natural
particles in air and soil to remove gaseous and particulate matter in
the hydrosphere, cryosphere, and atmosphere.
Smith: Understanding how
climate change impacts crop growth and soil health in Canada and
identifying ways to manage these impacts is especially important since
temperatures in Canada are increasing faster than the global average.
Historically we’ve seen how a warming climate can provide certain
benefits as the available seasonal crop heat units and frost-free
periods have increased over long-term historical averages. However, in
the future, some agricultural regions could be subject to higher
incidences of extreme drought, increased crop heat stresses and excess
water. In this presentation, we will review the state of models and
modelling procedures for predicting the impacts of climate change on
cropping systems. We will demonstrate how crops in Canada may respond
to climate change and discuss the benefits of adaptation by changing
crop types, rotations, and fertilizer strategies.
Kimbell:
Four years after the National Capital Region tornado
outbreak of
September 21, 2018, another summer convective storm affected southern
Ontario (including the NCR), on May 21, 2022. This time, while the
Northern Tornadoes Project did diagnose a few tornadoes, the storm’s
primary manifestation was not tornadic. Rather, a linear convective
system developed over southwestern Ontario, and maintained its linear
characteristics throughout its trajectory across southeastern Ontario,
the NCR, and into southern Quebec north of Montreal. Many people in
Ontario and Quebec suddenly became familiar with the word “derecho,”
which is Spanish for “straight ahead.” We will talk about derechos,
including climatology, differences with tornadoes, and more.
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