Marine Biology Fieldwork Essentials

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  • View profile for Roberta Boscolo
    Roberta Boscolo Roberta Boscolo is an Influencer

    Climate & Energy Leader at WMO | Earthshot Prize Advisor | Board Member | Climate Risks & Energy Transition Expert

    181,449 followers

    On 30 June 2026, the global ocean recorded its warmest temperature anomaly ever measured for that date.... Globally. 🌊 This visualisation, based on Copernicus Marine Service data, shows sea surface temperatures across almost the entire ocean are running above the long-term average, with the global anomaly reaching +0.5°C — a record for this time of year, in a dataset stretching back to 1993. Two of the signals I've been tracking closely this year are converging in this single map: 🌡️ The Mediterranean marine heatwave remains firmly in place 🌊 The equatorial Pacific, where developing El Niño conditions are adding further warmth on top of an already-hot ocean 📈 The historical trend line tells that this isn't a single spike, it's the continuation of a climb that has been steepening for years The ocean is the planet's great heat regulator, absorbing 90% of the excess energy trapped by greenhouse gases. It has spared land temperatures from rising even faster. But it comes at a cost: warmer waters intensify storms, disrupt marine ecosystems and fisheries, and prime the atmosphere for more extreme, more humid heat on land. 🌡️ None of this would be visible without sustained, near-real-time ocean observation. Copernicus Marine and Climate Change Services are what let us see a record forming as it happens, rather than discovering it in hindsight — turning raw data into the lead time that preparedness for extreme weather depends on. 🛰️ 🛰️ Data: European Union, Copernicus Marine Service & Copernicus Climate Change Service

  • View profile for Wendy Schmidt

    Philanthropist, Investor, Writer, Sailor. Working to make the world healthy, resilient and secure for all.

    11,526 followers

    The ocean needs a temperature check. With ocean warming putting coastal communities and ecosystems at risk from stronger storms and rising seas, @ClimateCentral created a new tool to measure how climate change is affecting sea surface temperatures on a daily basis. Climate Shift Index: Ocean (Ocean CSI), based on attribution science, will link human-caused climate change and ocean temperatures, which we know have been hotter every single month since April 2023. In one early case study, Ocean CSI shows that climate change made this summer’s Hurricane Beryl 400 times more likely to occur. Ocean CSI builds on Climate Central’s earlier effort to track how warming affects the weather around the world on a daily basis. And while sea surface temperatures may seem like a more distant concern than the weather we experience in our daily lives, the ocean is our life support system. It regulates climate and provides food and livelihoods for billions of people. As the ocean warms, it is less able to keep climate in check, nurture biodiversity or keep storms at bay. Thanks to Climate Central, we now have a precise and timely measure of ocean health. It’s up to all of us to take this information and act on it. https://lnkd.in/gbqRxgnX

  • View profile for Harold S.

    Battalion Commander | Artificial Intelligence | National Security Space

    13,345 followers

    Between 1985 and 1989, a warming of 0.06 C per decade was observed, while from 2019 to 2023, the sea-surface temperature rose by 0.27 C per decade. This suggests that sea surface temperatures are rising 4.5 times faster since 2019 than they were at the end of the 1980s. The study calculated monthly global mean sea-surface temperature using global satellite data records generated through ESA’s Climate Change Initiative (CCI). The dataset used observations from 20 infrared radiometers on board satellites including ESA’s ERS-1, ERS-2, Envisat, Copernicus Sentinel-3 and two microwave radiometers from 1980 to 2023 to provide a globally accurate temperature trend. The unprecedented warming was the finding of a study published in the journal Environmental Research Letters. The study attributes the rising sea surface temperature to increasing levels of greenhouse gases in the atmosphere. Lead author of the study, Chris Merchant, from Reading University, UK, explained that greenhouse gases trap heat in our atmosphere, resulting in an imbalance in the energy received by our planet from the Sun, and the energy radiated back out to space, resulting in an excess energy imbalance. He said, “This energy imbalance drives climate change. Given the accelerations in ocean warming and evolving climate dynamics, we need ongoing monitoring and data improvements to ensure our climate models can accurately reflect future temperature increases.” The study analyses various factors that influence the warming of the oceans, from weather phenomena such as El Niño, to volcanic eruptions. It found these phenomena cause short-term fluctuations in sea-surface temperatures but do not significantly interrupt the long-term warming trend. Owen Embury, co-author and scientific leader of the ESA-CCI sea-surface temperature project, which contributed the long-term data set, said, “Our study clearly identifies the increasing accumulation of planetary energy as the dominant driver of long-term sea surface warming, while short-term variations from El Niño, volcanic activity and solar changes add variability but do not alter the overall accelerating trend.” The results of the current study will contribute to ESA’s science exploitation project, MOTECUSOMA which is investigating Earth’s energy imbalance and its impact on climate change. Owen added, “Addressing these challenges requires accurate climate projections – increasing ocean heat uptake intensifies extreme weather events, disrupts ecosystems and accelerates sea level rise, making continued observation and model refinement essential.” The SST data record is available from the ESA CCI data portal. Versions formatted to support global climate modelling efforts are available via Obs4MIPs framework. #CCI #ESA #Satellites Global and precise records of sea surface temperature are crucial for tracking and understanding Earth’s energy imbalance. (ESA)

  • View profile for Tom Harris

    Climate Science Writer and Climate Advocate

    3,768 followers

    A thorough analysis based on multiple datasets produced by several independent research groups, finds that the oceans continued to warm rapidly in 2024, not only at the surface but also across the upper 2000m. About 90% of the heat accumulated in the climate system is stored in the ocean, increasing sea surface temperatures and Ocean Heat Content (OHC). OHC is therefore a key climate indicator for monitoring planetary warming. Due to the ocean’s large heat capacity and immense volume, the change in OHC is characterised by much smaller month-to-month and year-to-year fluctuations as compared to the surface temperatures, making OHC a robust metric of climate change. OHC is measured in Zetajoules (10 to the 21 Joules) or a sextillion joules. That’s a lot. 1 ZJ is 16 billion Hiroshima bombs worth of heat energy.  🤯 The global OHC changes within the upper 2000m ocean layer since 1958 show that there has been an unequivocal ocean warming trend in recent decades, regardless of the data sources and processing techniques. The upper 2000m of the world’s ocean has warmed on average by 6.4 ± 0.3 ZJ yr−1 during 1958–2024. There has been a two-to-three fold increase in the rate of OHC since the late 1980s. Since 2007, the upper 2000m ocean warming rate has been 11.1 ± 1.1 ZJ yr−1, 10.1 ± 1.2 ZJ yr−1, 12.3 ± 2.0 ZJ yr−1 for the IAP/CAS, Copernicus Marine, CIGAR-RT datasets respectively. The increase in the OHC rate in recent decades indicates a multi-decadal acceleration of ocean warming. 2024 saw an increase of 16 ZJ, another new record for this auspicious year. 🌊 Ocean warming substantially impacts the major Earth system components. For example, ocean warming accounts for more than 1/3 of the global mean sea level rise through thermal expansion, dominating regional sea level patterns. 🌪️ Ocean warming also exacerbates extreme weather and ocean events. These include intensification of typhoons, hurricanes, and marine heatwaves. The extra heat and moisture that enters into the atmosphere make storms more severe, with heavier rain, stronger winds, and more significant flooding. 🛟 Warming also leads to a more rapid intensification of storms and slower decay after landfall, increasing flooding risks related to tropical cyclones. 🐠 Warming is also a factor that can cause ocean deoxygenation which itself is a significant hazard for not only marine life and ecosystems, but also for humans and our terrestrial ecosystems.     🪸 Marine heatwaves can devastate corals driving bleaching events. 🌡️ Warm water also absorbs less carbon dioxide from the air, driving acceleration of the greenhouse effect. All these impacts were seen in 2024. Until we reach net-zero emissions, the ocean warming acceleration trend will continue (IPCC AR6), and OHC will likely continue to break records driving ever increasing weather impacts. Paper: https://lnkd.in/er3sxTtv #oceans #oceanheatcontant #climatechange #hurricane #SST #OHC 

  • View profile for Soniya panwar

    Former Project Intern at IIRS, ISRO || MSc Environmental science || Specialization in natural resource management || Forestry Graduate.

    2,900 followers

    🌊 Understanding the Trends in Sea Surface Temperature (SST) in the Indian Ocean. Over the past 20 years, the Indian Ocean has experienced notable variations in Sea Surface Temperature (SST), a critical factor influencing monsoons, cyclones, and marine ecosystems. By analyzing monthly mean SST for two key summer months (July, August) and two winter months (December, January) across all years, we can observe seasonal patterns and long-term trends. 🔥 Summer SST (July & August) The domain average SST for July is 28.51°C, while for August, it is 28.17°C. SST during these months exhibits higher temperatures in the equatorial and southern regions, with relatively lower temperatures near the Arabian Sea. The western Indian Ocean, particularly the Arabian Sea, shows a cooler pattern due to the Southwest Monsoon upwelling, where deep, cooler waters rise to the surface. ❄️ Winter SST (December & January) The domain average SST for December is 27.96°C, while for January, it is 30.01°C. The SST in December is relatively cooler, especially in the northern regions, as the Northeast Monsoon dominates. January shows an increase in SST, particularly in the equatorial and southern regions, reflecting a transition towards pre-summer warming. 📈 Long-Term Trends from Annual SST Time Series (2007-2023) The annual SST time series reveals a gradual warming trend in the Indian Ocean over the years. Despite inter-annual variations, the domain-averaged SST has seen an overall increase, aligning with global ocean warming trends. This warming could have significant implications for tropical cyclone activity, monsoon patterns, and marine biodiversity. 🌍 Why Does This Matter? 1️⃣ Climate Change Indicator – Rising SSTs indicate global warming and its regional impacts. 2️⃣ Cyclone Intensity – Warmer SSTs provide more energy for cyclones, making them stronger and more frequent. 3️⃣ Marine Ecosystems – Higher temperatures can lead to coral bleaching and disrupt marine biodiversity. Understanding SST trends is crucial for climate resilience, disaster preparedness, and sustainable ocean management. This analysis highlights the importance of continuous monitoring of our oceans to mitigate future climate risks. #ClimateChange #SeaSurafceTemperature #IndianOcean #Cyclones #TropicalCyclones #EnvironmentalScience #Oceanography #SSTAnalysis #TimeSeries #SustainableOceanManagement #DisasterManagement

  • View profile for Antonio Vizcaya Abdo

    Turning Sustainability from Compliance into Business Value | ESG Strategy & Governance Advisor | TEDx Speaker | LinkedIn Creator | UNAM Professor | +129K Followers

    129,185 followers

    Sea surface temperatures have been climbing steadily for past five decades ⬇️ The latest World Resources Institute graph shows that average sea surface temperatures have risen by more than 1°C above the 1861–1890 average, with the sharpest increase occurring since the 1970s. The severity of this trend becomes clearer when we consider the role of the ocean in regulating the global climate. The ocean has absorbed around 91% of the excess heat accumulated in the climate system. It has also absorbed a significant share of human-generated carbon dioxide, helping to slow the pace of warming in the atmosphere. Without this enormous buffering capacity, the climate crisis would already be considerably more severe. However, the ocean is paying the price. As more heat accumulates, marine heatwaves intensify, coral reefs bleach, oxygen levels decline, species move toward cooler waters and fisheries face growing disruption. Warmer waters also contribute to sea level rise, influence rainfall patterns and increase the potential intensity and rainfall of tropical storms. The consequences extend far beyond marine ecosystems. Billions of people depend on healthy oceans for food, employment, trade, transportation and protection from coastal hazards. Ports, tourism, fisheries, infrastructure, insurance markets and entire coastal economies are exposed to changes already unfolding beneath and above the surface. The ocean is one of our strongest allies in coping with the climate crisis, but its ability to continue absorbing heat and carbon cannot be treated as unlimited. Protecting and restoring marine ecosystems, reducing emissions rapidly, strengthening coastal adaptation and incorporating ocean risks into business and public policy must move much higher on the climate agenda. The ocean has helped shield humanity from the full force of global warming. The graph shows how much pressure that shield is now carrying. Source: World Resources Institute, based on Met Office Hadley Centre data.

  • View profile for Afed Ullah Khan, PhD

    Hydrologist | Climate Change & Water Resources Researcher | Remote Sensing & AI for Sustainable Development | GIS, GEE, Python, R | Consultant GIZ, UNICEF & Adam Smith International

    3,920 followers

    🌍 Visualizing Ocean Temperature Trends: A Python Approach 🌊 Climate scientists and researchers are constantly working to understand the impacts of global warming on the oceans. One of the essential tools in this process is data visualization. Using Python, we can create compelling, clear visualizations that help us interpret complex ocean temperature trends across latitudes and depths. 📊 In this example, I generated zonal mean ocean temperature trends from 1958 to 2024, considering latitudes from -60° to 60° and depths ranging from the surface to 2000 meters. The visualization highlights: 1️⃣ Temperature trends that show how ocean temperatures have warmed or cooled over time. 2️⃣ Climatological mean temperature contours to compare with observed trends. 3️⃣ Interactive visualizations that help researchers, policymakers, and educators better understand the depth of climate change impacts on ocean temperatures. 💻 Python Libraries Used: Matplotlib: For plotting contour maps and color gradients. NumPy: To generate synthetic data for trends. Data visualization is key in communicating complex climate patterns, and with Python, we can turn raw data into accessible stories that inform critical climate discussions.🔍 #DataScience #ClimateChange #Python #OceanTemperature #ClimateVisualization #DataAnalysis

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