We have applied the TEX86 paleothermometer to produce a surface water temperature record for Lake Malawi spanning the past 700 years. Over much of the record temperature fluctuates from similar to 24-27 degrees C with a mean of similar to 25 degrees C however, there has been a substantial increase in temperature of similar to 2.0 degrees C during the past similar to 100 years. The TEX86 temperature record reveals a strong similarity to the instrumental record: both records demonstrate warming (similar to 0.7-1.4 degrees C) over the past similar to 50 years as well as a cooling anomaly around 1959. Comparison of the TEX86 temperature record with the proxy records of primary productivity suggests that wind induced upwelling and/or precipitati...
The role of the tropics in global climate change is actively debated, particularly in regard to the...
Africa\u27s climate became progressively drier and more variable in the last few million years (e.g....
African climate changed considerably throughout the Pleistocene (2.588 million (Ma) to 12 thousand y...
We have applied the TEX86 paleothermometer to produce a surface water temperature record for Lake Ma...
We have applied the TEX86 paleothermometer to produce a surface water temperature record for LakeMal...
Wepresent a TEX86-derived surfacewater temperature record for LakeMalawi that provides the first con...
High-resolution profiles of the mass accumulation rate of biogenic silica and other geochemical prox...
Lake Tanganyika, the deepest and most voluminous lake in Africa, has warmed over the last century in...
Lake Malawi is the third largest lake in Africa and plays an important role in water supply, hydropo...
Century-to-millennial scale climatic variability in Lake Malawi revealed by isotope records. 1
African climate is generally considered to have evolved towards progressively drier conditions over ...
African climate is generally considered to have evolved towards progressively drier conditions over ...
African climate is generally considered to have evolved towardsprogressively drier conditions over t...
Diatom-based oxygen isotope data (δ18Odiatom) from Lake Malawi show multi-centennial scale wet–dry i...
A growing number of proxy, historical and instrumental data sets are now available from continental ...
The role of the tropics in global climate change is actively debated, particularly in regard to the...
Africa\u27s climate became progressively drier and more variable in the last few million years (e.g....
African climate changed considerably throughout the Pleistocene (2.588 million (Ma) to 12 thousand y...
We have applied the TEX86 paleothermometer to produce a surface water temperature record for Lake Ma...
We have applied the TEX86 paleothermometer to produce a surface water temperature record for LakeMal...
Wepresent a TEX86-derived surfacewater temperature record for LakeMalawi that provides the first con...
High-resolution profiles of the mass accumulation rate of biogenic silica and other geochemical prox...
Lake Tanganyika, the deepest and most voluminous lake in Africa, has warmed over the last century in...
Lake Malawi is the third largest lake in Africa and plays an important role in water supply, hydropo...
Century-to-millennial scale climatic variability in Lake Malawi revealed by isotope records. 1
African climate is generally considered to have evolved towards progressively drier conditions over ...
African climate is generally considered to have evolved towards progressively drier conditions over ...
African climate is generally considered to have evolved towardsprogressively drier conditions over t...
Diatom-based oxygen isotope data (δ18Odiatom) from Lake Malawi show multi-centennial scale wet–dry i...
A growing number of proxy, historical and instrumental data sets are now available from continental ...
The role of the tropics in global climate change is actively debated, particularly in regard to the...
Africa\u27s climate became progressively drier and more variable in the last few million years (e.g....
African climate changed considerably throughout the Pleistocene (2.588 million (Ma) to 12 thousand y...