Results 1 to 10 of about 419 (169)

The Indonesian Throughflow circulation under solar geoengineering [PDF]

open access: yesEarth System Dynamics, 2023
The Indonesia Throughflow (ITF) is the only low-latitude channel between the Pacific and Indian oceans, and its variability has important effects on global climate and biogeochemical cycles.
C. Shen   +4 more
doaj   +3 more sources

Change in Salinity of Indonesian Upper Water in the Southeastern Indian Ocean during Argo Period [PDF]

open access: yesHeliyon, 2022
The change in salinity of Indonesian Upper Water (IUW) in the Indian Ocean has been examined during 2004–2020 based on the Argo product. Monthly salinity fields reveal a contrast of IUW salinity changes between two time periods (2004–2013 and 2014–2020 ...
Mochamad Riza Iskandar, Toshio Suga
doaj   +2 more sources

Genetic Diversification in a New Guinean Frog Genus (<i>Mantophryne</i>, Microhylidae) was Driven by Ancient Tectonic Activity and Climate Reorganisation. [PDF]

open access: yesEcol Evol
Our dated phylogeny and biogeographic analysis of Mantophryne, a microhylid frog genus endemic to New Guinea, revealed origins in the East Papuan Composite Terrane (EPCT) in the late Pliocene. Dispersal and diversification out from the EPCT was driven by tectonic activity and climate reorganisation, creating habitat corridors and isolations in the Late
Morris RS   +5 more
europepmc   +2 more sources

Post‐Hiatus Enhancement of ENSO Forecast Skill via Salinity‐Mediated Indo‐Pacific Inter‐Basin Coupling

open access: yesGeophysical Research Letters
The El Niño–Southern Oscillation (ENSO) predictability has notably declined since the 1998–2013 global warming hiatus, challenging conventional sea surface temperature (SST)‐based forecast models.
Jing Wang   +3 more
doaj   +2 more sources

Shotgun metagenomic dataset of microbial communities in the water column of the Flores Sea, IndonesiaNCBI [PDF]

open access: yesData in Brief
The Flores Sea is a crucial component of the Indonesian Throughflow (ITF) pathway, which influences the transport of carbon, oxygen, and nutrients that support marine ecosystems. Here, we present the first dataset of microbial communities from the Flores
Buntora Pasaribu   +8 more
doaj   +2 more sources

Opposite Trends of Eddy Kinetic Energy in the Tropical Indo‐Pacific Ocean Since the 1990s

open access: yesGeophysical Research Letters
Oceanic mesoscale eddies are pivotal in redistributing mass and heat. Despite a warming‐induced increase in global oceanic stratification, previous studies have reported a global increase in mesoscale eddy activity, particularly in eddy‐rich regions ...
Xinying Guo   +6 more
doaj   +2 more sources

Significant Southern Hemisphere contribution to the Indonesian Throughflow over the last 800,000 years [PDF]

open access: yesNature Communications
The low-latitude flow of water masses from the Pacific to the Indian Ocean, the Indonesian Throughflow (ITF), is a choke point of the surface ocean return flow of the ocean conveyor belt.
Markus Kienast   +6 more
doaj   +2 more sources

Lithic Miniaturization Provides a Signature of an MIS4-3 Southern Dispersal of Homo sapiens. [PDF]

open access: yesEvol Anthropol
ABSTRACT Fossil and artefactual evidence shows Homo sapiens in Eurasia well before 75 ka. However, genetic evidence suggests all extant non‐African populations derive almost all of their ancestry from a dispersal that only diverged in the last 60–50 ka. In northern Eurasia, the Upper Paleolithic with its laminar blade knapping provides an archeological
Shipton C.
europepmc   +2 more sources

Bipolar Oceanic Processes Drive Indonesian Throughflow Decline Under Climate Warming

open access: yesGeophysical Research Letters
Climate models consistently project a weakening Indonesian Throughflow (ITF) under future warming, but its driving mechanisms remain incompletely explained.
Weihao Wang, Shantong Sun, Lixin Wu
doaj   +2 more sources

Metagenomic analysis of deep-sea bacterial communities in the Makassar and Lombok Straits [PDF]

open access: yesScientific Reports
The extreme conditions of the deep-sea environment, including limited light, low oxygen levels, high pressure, and nutrient scarcity, create a natural habitat for deep-sea bacteria.
Zen Ladestam Siallagan   +9 more
doaj   +2 more sources

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