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GFDL Research Highlights

June 14th, 2024 - Crucial role of sea surface temperature warming patterns in near-term high-impact weather and climate projection

Recent studies indicate that virtually all global climate models have difficulty simulating observed sea surface temperature (SST) trend patterns over the past four decades. Models produce enhanced warming in the eastern Equatorial Pacific (EPAC) and Southern Ocean (SO) warming, while observations show intensified warming in the Indo-Pacific Warm Pool (IPWP) and slight cooling in the eastern EPAC and SO. Read More…

June 12th, 2024 - Skillful seasonal prediction of wind energy resources in the contiguous United States

This study explored the extent to which the strong year-to-year variations of wind energy resources in the contiguous United States may be predictable using GFDL’s SPEAR seasonal prediction system. The authors demonstrate SPEAR’s capability for predicting the observed strong year-to-year variations of spring wind energy resources with great skill over the Southern Great Plains, in which more than half of the total U.S. wind capacity is located. SPEAR also can provide state-level spring wind energy prediction with a correlation skill reaching 0.8 for Texas, which alone accounts for almost a quarter of the total U.S. wind capacity. These skillful seasonal wind energy predictions at the regional scale or state level can provide valuable information over the Great Plains for coping with year-to-year variations and optimizing wind energy production. Read More…

May 28th, 2024 - Cloud radiative effects associated with daily weather regimes

This research Investigates the effect of high-impact storms on Earth’s radiation budget, in order to better constrain climate models and improve weather and climate forecasts. Using detailed satellite observations and reanalysis data, the author categorized daily weather patterns into different types and measured the cloud radiative effects (CRE) associated with each type. The weather patterns included non-precipitation days, drizzle, wet non-storm days, and storm days, encompassing events like atmospheric rivers, tropical storms, and mesoscale convective systems. Read More…

May 20th, 2024 - The GFDL variable-resolution global chemistry-climate model for research at the nexus of US climate and air quality extremes

In the U.S., air pollution includes contributions from multiple local human and natural sources, as well as transported sources like wildfire smoke from Canada, dust plumes from Africa, and intercontinental pollution from Asia. Accurate projection of future climate and air quality at scales relevant to local and regional stakeholders requires a seamless modeling system that can provide detailed information over a targeted region, while still integrating the global Earth system components in a computationally efficient manner. Scientists at GFDL have developed a novel variable-resolution global chemistry-climate model, known as AM4VR, for research at the nexus of U.S. climate and air quality extremes. Read More…

April 29th, 2024 - Poleward intensification of midlatitude extreme winds under warmer climate

Given the significant risks posed by near-surface extreme wind speeds associated with midlatitude cyclones to lives, livelihoods, and infrastructure, it is imperative to understand their physical changes, including magnitudes and patterns, under human-induced global climate change. This study used GFDL’s high-resolution (50 km grid-spacing) atmospheric climate model, AM4, to investigate the global impact of midlatitude cyclones on extreme wind speed events, in both hemispheres, under a warmer climate. The authors conducted simulations covering the period 1949–2019 for both the present-day climate and an idealised future global warming climate scenario with a sea surface temperature (SST) increase of 2 K. Read More…

March 28th, 2024 - Kilometer-scale global warming simulations and active sensors reveal changes in tropical deep convection

Under global warming, changes in the location and structure of the deep convection in the tropics have profound consequences for tropical climate. The tropics are characterized by the ubiquitous presence of high ice clouds formed by detrainment from precipitating deep convection. The bulk of these clouds are so-called anvil clouds in extensive formations that shield the convective centers.  These can persist for several hours after the decay of active convection and they carry low to moderate ice loads. Read More…

February 15th, 2024 - Impacts of the North Atlantic biases on the upper troposphere/lower stratosphere over the extratropical North Pacific

The interplay between the ocean and atmosphere plays a crucial role in shaping weather patterns and temperatures around the world. Yet, the winter upper troposphere/lower stratosphere (UTLS) temperature/vertical motion response over the extratropical North Pacific induced by North Atlantic changes is not well understood. Using GFDL’s high-resolution climate model CM2.5, the authors corrected the North Atlantic Ocean circulation biases to unravel the wintertime atmospheric impacts. Read More…

February 8th, 2024 - Ocean biogeochemical fingerprints of fast-sinking tunicate and fish detritus

Marine ecosystems play a critical role in the global carbon cycle through the food web regulation of air-sea carbon fluxes and the transfer of particulate matter from the upper oceans to depth. Recent evidence has suggested that the detritus from fishes and gelatinous zooplankton, specifically the pelagic tunicates such as salps and pyrosomes, may have a disproportionate impact on the ocean’s biological pump due to them sinking approximately ten times faster than bulk detritus. These fluxes result in increased sequestration of particulate carbon and nutrients into the deep oceans, but their impact on biogeochemical cycles at depth is poorly understood. Read More…

December 22nd, 2023 - The importance of dynamic iron deposition in projecting climate change impacts on Pacific ocean biogeochemistry

Projections of future nutrient limitation and primary production have implications for fisheries management. The authors used GFDL’s Earth system model, ESM4.1, to explore climate-driven changes in the deposition of dust and iron from the atmosphere to the ocean under a range of climate change scenarios, in an attempt to understand where the “fish food” is going to be and why. Read More…

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