Articles tagged with Paleoclimatology
Researchers are using tree rings and sediments to reconstruct Atlantic hurricane history over millennia. By combining these natural archives with global climate model simulations, they aim to refine the record of history's hurricanes.
A new study found that birds and mammals evolved into new species at higher rates where the land has risen most over the past three million years. This effect was found to be greater than historical climate change, present-day elevation, and temperature in driving speciation.
Researchers from the Institute of Atmospheric Physics found that tropical Pacific decadal variability and Atlantic multidecadal variability drive Central Asian precipitation changes. Warmer SSTs in these regions favor wetter conditions, especially in southern and northern parts of Central Asia.
Research from UBC and HKU Earth scientists reveals that massive volcanism played a key role in triggering oceanic anoxia, with CO2-induced environmental warming creating 'dead zones' over short timescales. The findings provide important insights into the sensitivity of the Earth system to global biogeochemical cycles and marine biology.
Researchers reconstructed Mongolia's temperature history using a new tree ring analysis method, confirming record-breaking summer warmth over the past eight centuries. The study supports the delta blue intensity method and enhances climate projections, highlighting the urgent need to address Central Asia's rapid warming.
Researchers observed a 'warming bias' in the Earth's ancient history, with more warming events and greater temperature shifts than cooling events. The study suggests that a multiplier effect may kick back in as ice sheets disappear, leading to further amplification of human-induced global warming.
A new study reveals that the domestication of plants and construction of settlements based on agriculture in ancient Japan coincided with periods of relatively warm and stable climate. This challenges the conventional theory that a climatic cooling event drove humans to adopt agriculture.
A massive volcanic eruption in Indonesia about 74,000 years ago likely caused severe climate disruption globally, but early human populations were relatively unaffected. The study suggests that regional variation in climate impacts occurred, with the Northern Hemisphere experiencing cooling of at least 4°C.
The study suggests that the tropical rain belt's latitudinal oscillation range contracted, resulting in reduced rainfall in Brazil's Northeast region. This finding can help predict the region's future climate and inform strategies for managing food and water security.
Researchers used a new technique to reconstruct the climate of Europe during the Cretaceous period, finding that temperatures fluctuated between 15°C and 27°C. This shows that seasonal differences remained constant despite rising average temperatures, leading to hotter summers and warmer winters.
The study reveals that researchers' subjective decisions can lead to variations in climate reconstruction outcomes. The experiment showed notable differences in amplitude and sensitivity among multiple reconstructions using the same raw data. To improve reliability, teams are advised to create ensemble reconstructions.
A new study reveals that the End-Permian extinction event, also known as the 'Great Dying', was caused by a rapid spike in global temperatures due to volcanic activity. The researchers found that the region experienced abrupt aridification and changed climate patterns, with high-southern latitudes serving as refugia for moisture-loving...
Researchers present a new framework for studying 'the History of Climate and Society,' which reveals that past populations adapted by exploiting opportunities and resilient energy systems. Case studies show that societies like the Roman Eastern Mediterranean thrived under adverse climate conditions.
A global climate dynamic study suggests that shifts in the Southern Hemisphere westerly wind belt can trigger rapid, global changes in atmospheric temperature. This 'Zealia Switch' mechanism relates to ocean currents and heat engine releases, influencing glacier growth.
A research team from the University of Miami used a 600-year-old marine sponge to reconstruct Atlantic Ocean temperatures, showing past volcanic activity and current global warming trends. The study's findings provide valuable insights into the impact of human activities on climate change.
Fossil discovery provides insights into ancient Tibetan biota and land surface height in the middle Eocene. The study reveals a diverse and humid subtropical forest ecosystem at an elevation of 1,500 meters under a monsoonal climate.
Researchers recommend using past climates to evaluate and fine-tune climate models, as they often perform better with historic climates but struggle with ancient climates. This could help narrow uncertainties surrounding future temperature, ice sheet, and water cycle changes.
Researchers discovered a 190-year lag between Greenland's relative warmth and mild winters at the Black Sea, suggesting thermal adjustment of the ocean interior. Enhanced precipitation and warm lake temperatures followed.
Researchers from ETH Zurich and colleagues reconstructed the Paleocene and Eocene climates using siderite minerals, finding high humidity and heat transport. This suggests today's global warming is linked to increased moisture and heat transport in the atmosphere.
A 14,000-year paleoecological reconstruction found that seabird establishment led to changes in Falkland Islands ecosystems through guano deposition. This terrestrial-marine link is critical for grasslands conservation efforts, as nutrients from marine ecosystems enrich the islands' nutrient-poor soil.
Researchers reconstructed Oligocene sea surface temperatures and found a warm global climate despite low atmospheric CO2 levels. The findings challenge existing understanding of greenhouse climates in the past and shed light on Earth's surface temperature evolution.
An international team publishes a global reference curve in Science, reconstructing the Earth's climate since the last great extinction 66 million years ago. The study provides a detailed understanding of past climate dynamics and recurring patterns, allowing for more accurate dating and correlation of climate events.
Scientists compiled a continuous, high-fidelity record of Earth's climate history extending 66 million years into the past. The record shows that natural climate variability due to changes in Earth's orbit around the sun is relatively small compared to projected future warming.
A new study reveals that abrupt climate warming events in Greenland during the last glacial period were synchronous with other rapid climate changes across the globe. The findings suggest that Arctic warming events triggered rapid climate change on a global scale.
Researchers have developed a framework to reconcile discrepancies in ancient sea surface temperature estimates and climate model results. By accounting for location-biased paleoclimate data, scientists can better reconstruct global climate conditions in the past and improve predictions of future climate scenarios.
A recent study evaluates proxy-based reconstructions and model simulations for past temperature changes, finding that uncertainties increase over time. The results show that climate modeling results are less reliable than proxy-based reconstructions, especially during Medieval times.
Jan Esper will track tree growth at 100 sites in the Northern Hemisphere to develop a new model for reliable climate data. This project aims to overcome the divergence problem, which undermines the reliability of temperature reconstructions based on tree rings.
According to new research, Gulf coast mollusks were able to survive past periods of climate change, including the Paleocene-Eocene Thermal Maximum (PETM), which warmed the planet by 9-14 degrees Fahrenheit. The study suggests that these resilient communities may adapt again to today's climate change.
A new study reveals that climate conditions, not human activity, dominated the shaping of early forests in New England for thousands of years. The research team combined archaeological records with studies on vegetation, climate, and fire history to reconstruct historical changes to the land.
Researchers found that temperatures exceeding present levels longer than during past interglacials suggest the Greenland Ice Sheet's fate is influenced by duration of warming. The study suggests a possible threshold for significant GIS retreat may be less than 1 °C above current levels.
The last known tropical glaciers in the West Pacific Warm Pool are at risk of disappearing within a decade. The study found that the Puncak Jaya glaciers in Indonesia lost around 1.05 meters of ice per year between 2010 and 2015, with thinning rates increasing five-fold during strong El Niño events.
A speleothem δ18O record from Klang Cave in southern Thailand shows decreased rainfall in the northern-central Indo-Pacific (NCIP) region. The study also found that anthropogenic forcing of rainfall may be indistinguishable from natural variability during certain climate periods.
Eastern Canada's climate was characterized by a warm temperate and fully humid climate, with mean annual temperatures around 15°C. This new information is useful for studying the evolution of the region's climate and its relevance to today's changing climate.
Scientists discovered ancient crocodile species' climate sensitivity, suggesting they served as 'climate clocks.' Fossil analysis mapped their distribution to reconstruct global temperatures during the Eocene-Oligocene epochs. The study provides new insights into how these ancient reptiles adapted to changing climates.
A study from U of T Mississauga uses new techniques to reconstruct summer temperatures over the last 13,600 years, confirming current global warming trends. The research reveals that recent climate warming in the central Yukon region has surpassed the warmest temperatures experienced in the previous 13,600 years.
A recent study examines California's climate over a centuries-long time period, linking long-term wind patterns to future wildfire risks. The research provides a stronger foundation for evaluating regional natural hazards in the state.
Geoscientists at UMass Amherst have reconstructed the longest and highest-resolution climate record for the Northeastern United States, revealing previously undetected past temperature cycles. The study used branched glycerol dialkyl glycerol tetra ethers (branched GDGTs) to provide an independent terrestrial paleo-thermometer.
Researchers from the University of Barcelona used chironomid subfossils to reconstruct Holocene temperatures in the Iberian Peninsula, showing a rise in temperatures during the Holocene Climate Optimum and a decline after its onset. The study provides a promising tool for understanding climate evolution and natural changes.
Researchers at University of Basel developed new approach to analyze microbial molecular fossils in lake sediments, providing reliable temperature estimates. The study's findings can be applied globally, offering improved predictions for future climate conditions.
Researchers reconstructed a drastic climate change event in southern France using tree-ring width measurements and chemical analyses. They found that the region experienced increased air mass transport from the North Atlantic and regional variability in precipitation, leading to extreme weather conditions.
Researchers analyzed gomphotheres' tooth fossils for dietary patterns, finding evidence of tree browsing and herb grazing. The study suggests that the mammals' diets were flexible according to resource availability and latitudinal climate gradients.
Researchers found that the northern Galápagos Islands have been warming by almost 0.4 degrees F per decade, with temperatures increasing overall by about 1.1 degrees F since the 1970s. This finding is significant because it suggests that the region's reefs are more vulnerable to climate change than previously thought.
A study reconstructing climatic patterns in China from AD 1-1911 found long periods of cold and dry conditions associated with epidemic outbreaks. However, the relationship between temperature and epidemics varied across short time scales, highlighting climate's scale-dependent impacts on disease prevalence.
A GW researcher argues that the human genus may have originated by chance, rather than in response to environmental changes. Computer simulations suggest that clusters of species originations could be caused by random fluctuations, rather than a single broad-scale event.
The RegCM4 model simulates China's climate well, reproducing present-day climatology and interannual variabilities. However, it exhibits biases in winter temperatures and precipitation, with underestimation of heavy rainfall events and overestimation of consecutive dry days.
Researchers have developed a new method to analyze the carbon content of ancient coccolithophore shells, providing insights into past CO2 levels and climate sensitivity. The study uses mathematical modeling and laboratory experiments to understand the biology of ancient creatures and their impact on the environment.
A new study in Paleoceanography reveals that the last time Earth was as warm as it is today, a melting Greenland Ice Sheet circulated cold freshwater in the Atlantic Ocean as far south as Bermuda. This circulation elevated sea levels and altered ocean climate and ecosystems.
A Vanderbilt University team is using mineral deposits in caves to shed new light on prehistoric megadroughts in the western US. The researchers hope to identify atmospheric drivers that caused extended droughts, informing projections of future drought severity.
Researchers at UTA examine global warming events during the Early Paleogene period, which occurred 66-45 million years ago. They aim to understand the effects of greenhouse gas emissions on life on Earth and provide analogs for current climate change.
Researchers are reconstructing past temperature and hydrology records in southern Greenland using high-resolution quantitative methods. This project sheds light on climate variations during the period of Norse settlement, which had been abandoned by the early 15th century due to various factors.
Marina Suarez aims to understand how the Earth functions with high levels of carbon dioxide and how it recovers from extreme conditions. Her research in paleoclimatology will inform current studies on climate change, a pressing global concern.
A new study finds that carbon emissions will have long-lasting impacts on the planet, with some effects lasting over 100,000 years. The researchers warn that reducing emissions slightly or significantly is not sufficient to prevent catastrophic consequences.
The analysis highlights the importance of considering long-term impacts of climate change, which can last tens of thousands of years. Reducing emissions slightly or significantly is not sufficient, with the target being zero or negative carbon emissions as soon as possible.
Recent studies show a connection between the Earth's tilt and the movement of the Intertropical Convergence Zone, the world's heaviest rainbelt. This new information enables climate scientists to better predict extreme weather events and has implications for global climate and sustainable human socioeconomic development.
Junior Professor Denis Scholz will continue speleothem research, extending it to longer-term objectives. Speleothems are suitable archives of past climate variability due to their global distribution and precise dating capabilities.
A new study found that California's 6th-grade science textbooks give climate change a mixed message, presenting it as a controversial debate and downplaying the role of humans. The textbooks do not accurately reflect the scientific consensus on human-caused global warming.
Researchers at University of Zurich predict up to 30% less precipitation in the Central Andes by 2100, exacerbating seasonal water shortages. The study suggests stronger westerly winds will lead to greater aridity, impacting the region's climate.
Researchers are refining their understanding of ice sheet response to warming, which will inform projections of sea-level change. A new era of climate modeling has begun, with improved estimates of Greenland and Antarctic ice sheet loss for given temperature increases during past warm periods.
Researchers found that lower oxygen levels led to increased precipitation and warmer temperatures due to the resulting drop in atmospheric density. The study's findings suggest that changes in oxygen concentrations may help explain features of past climates not accounted for by variations in carbon dioxide levels.
A recent paper by University of South Carolina paleoceanographer Kelly Gibson shows that rapid climate change affected marine ecosystems in the Cariaco Basin, a body of water off Venezuela's coast. The study used nitrogen isotope ratios to estimate changes in primary productivity and carbon sequestration in the ocean.